The results of the application of mobile direct-prospecting technology of frequency-resonance processing and interpretation of satellite images and photographs at the sites of hydrogen production, drilling wells, as well as within areas of hydrogen degassing in various regions are presented. Experimental reconnaissance studies were carried out to study the features of the deep structure of the hydrogen degassing areas.
The developed mobile and low-cost technology include modified methods of satellite images and photo-images frequency-resonance processing and decoding, vertical electric-resonance scanning of a cross-section, as well as a method of integrated assessment of oil and gas potential of large prospecting blocks and license areas. Separate methods of direct-prospecting technology are based on the principles of the “substance” paradigm of geophysical research, the essence of which is searching for a specific substance - oil, gas, gas condensate, etc.
The materials of instrumental measurements indicate that in regions of basalt volcano's location with roots at different depths, signals at hydrogen frequencies are almost always recorded. When scanning the cross-section, responses from hydrogen are recorded from the upper edges of basaltic volcanoes to their roots. It can be assumed that basaltic volcanoes are a kind of channel through which hydrogen migrates to the upper horizons of the cross-section and further into the atmosphere. Within many basaltic volcanoes at a depth of 68 km, deep (living) water is synthesized. Hydrogen-rich water is curative and can be used for wellness purposes. All surveyed zones of longevity on Earth are located within basalt volcanoes, in which water synthesized at a depth of 68 km migrates to the surface and is used for water supply. Hydrogen deposits can be formed by basaltic volcanoes in adjacent sealed reservoirs. Within some survey areas, responses at hydrogen frequencies from limestones, dolomites, and marls were recorded at shallow depths. Hydrogen deposits formed near basalt volcanoes in different types of reservoirs can be discovered and localized during areal exploration using proven methods. Direct-prospecting technology can also be used to study reservoirs in crystalline rocks (basalts including). Detailed studies and wells drilling in promising areas can be planned and carried out for hydrogen and living water at the same time.
The result of the investigation indicates the advisability of using direct-prospecting methods of frequency-resonance processing of satellite images to detect zones of hydrogen accumulation in areas of basalt volcanoes location, as well as in areas of hydrogen degassing. The use of mobile and low-cost technology will significantly speed up the exploration process for hydrogen, as well as reduce the financial costs for its implementation.
Results of reconnaissance survey _Profile TESZ-2021_FINAL_short version.pdfDr. Arzu Javadova
The results of a reconnaissance survey of a seismic profile on Ukraine territory are presented. Experimental studies were carried out with the aim of additional approbation of direct-prospecting methods and improvement of methodological techniques of their application in the exploration process for oil, gas and natural hydrogen, as well as in the study of the deep structural elements of the Earth. The results indicate that it is promising for the detection of HC deposits in the cross-section and the expediency of carrying out prospecting works of a detailed nature within it. In the northern part of the research area, by instrumental measurements a basalt volcanic complex has been localized, which is promising for of natural hydrogen and living water accumulations searching in the cross-section. During the cross-section scanning, responses at gas frequencies were recorded without interruption up to 5 km, which may indicate the presence of a deep channel within the surveyed area, through which oil, condensate and gas migrate to the upper horizons of the cross-section. The results of the survey indicate the advisability of direct-prospecting methods and technologies using when studying the deep structure of small areas and large blocks by geoelectric and seismic methods.
NMR water exploration & presentation of water project technology Fands-llc
The technology will be able to remotely detect and assess groundwater accumulation and flows anywhere on Earth to a depth of 5 km directly.
At a time of deep recession in the global industry and staff reduction, only NMR technology will allow companies to maintain their exploration and prospecting programs scheduled for 2020 at a symbolic price.
( NMR technology provides acquisition of absolute field data with efficiency 2.5-3.0 times higher than indirect seismic data and at a price ten times lower than 2D/3D seismic data).
And most importantly, we are operating remotely, we are not afraid of the coronavirus pandemic all over the world!!!
We will search for reserves and water flows remotely with high accuracy anywhere in the world:
- the identification and contouring of accumulations and flows of underground fresh water,
- mapping the contours;
- obtaining the number of horizons and the depth of their occurrence;
- determining thickness aquifers and reservoir rocks,
- Determination of promising drilling points.
The NMR technology is based on the phenomenon of resonance, which allows direct detection and contouring of accumulations and flows, like the MRI scanning in medicine, which allows seeing human body problems at once.
RESULTS OF THE APPLICATION OF DIRECT-PROSPECTING TECHNOLOGY OF SATELLITE IMAG...Dr. Arzu Javadova
The results of reconnaissance studies within the Shakal and Halabja exploration blocks in Kurdistan are presented. Experimental studies were carried out using a mobile direct-prospecting technology, including modified methods of frequency-resonance processing and decoding of satellite images and photo images, vertical electric resonance scanning of the cross-section and a method of integral assessment of the oil and gas potential of large prospecting blocks and license areas. At the local survey site within the Shakal block, responses from oil, condensate, phosphorus and limestone were recorded. The lower boundary of the limestones was established at a depth of 4676 m. By scanning the cross-section from 2770 m, step 1 cm, the responses of oil from limestones were obtained from the intervals: 1) 2771-2794 m, 2) 2795.3-2815.45 m, 3) 2834.40-2854 m. During processing the image of the entire Halabja block, signals were recorded at the frequencies of oil, condensate, phosphorus gas, bacteria, sodium chloride and dolomite. At the 57 km hydrocarbon synthesis boundary, responses from oil, condensate and gas were recorded. When scanning the cross-section from 480 m to 4 km, step 50 cm, responses from oil were obtained from two intervals: 1) 1140-1200 m, and 2) 3310-3340 m. Within the local fragment of the block by scanning up to 5 km with a step of 1 m responses of oil from salt were recorded from the intervals: 1) 295-350 m, 2) 1190-1260 m, 3) 2015-2320 m). The response intervals within the 1st and 3rd horizons have been refined by scanning with a step of 5 cm. The results of experimental studies show that practical application of direct-prospecting methods and technologies will accelerate and optimize the exploration process for oil and gas.
Within the framework of a new, "substance" (“matter”) paradigm of geophysical research, a "direct" search for a specific physical substance is carried out: gas, oil, gas hydrates, water, ore minerals and rocks (gold, platinum, silver, zinc, uranium, diamonds, kimberlites, etc.). The initial stage in the development of this paradigm can be considered the first research and development on the "direct" methods for oil and gas searching.
Subsurface Determination Of Cavities In Limestone Rock Area By Geoelectric Me...IJERA Editor
Two Dimensional of geoelectric method can be used to find out the conductive formation in the earth surface. The purpose of this research is to give the description about the geological subsurface formation, that the high resistivity value is indicate the potential area of cave and void in the limestone rocks. The dipole dipolegeoelectric method is used in this research with the path of lines is 250 m with 10 m electrode spacing. The total lines is 7 and the azimuth is from east to west. Resistivity method is started with inject the electrical current into the earth by current electrode, then potential difference will arise and measured by potential electrode. Variation value of resistance for each layer rock can calculated by divided potential defference with current value. The existence of the cavity is known by the resistivity value is more than 2500 ohm-m, while the cracks have a resistivity of 1500 to 2500 ohm-m.
The Sinkhole Occurrence Risk Mitigation in Urban Areas for the Historic Salt ...IEREK Press
The present research focuses on the definition of a novel methodology for sinkhole risk assessment above shallow salt mines. The research were carried out on the area above the Wieliczka salt mine, a World Heritage site. The study of vertical stresses on the basis of a theoretical state of rock mass deformation in the area of test chambers was performed. Furthermore, the risk of chamber collapse due to ventricular stress exceeding the limit specified in the zone were calculated based on the arch pressure theory. The final stage of the research consists of spatial analysis that leading to the identification of chambers potentially influenced by other risk factors. The research shown in the article strongly suggests that combined spatial analysis with geotechnical analysis may lead to reliable sinkhole risk assessment methodology.
The Sinkhole Occurrence Risk Mitigation in Urban Areas for the Historic Salt ...IEREK Press
The present research focuses on the definition of a novel methodology for sinkhole risk assessment above shallow salt mines. The research were carried out on the area above the Wieliczka salt mine, a World Heritage site. The study of vertical stresses on the basis of a theoretical state of rock mass deformation in the area of test chambers was performed. Furthermore, the risk of chamber collapse due to ventricular stress exceeding the limit specified in the zone were calculated based on the arch pressure theory. The final stage of the research consists of spatial analysis that leading to the identification of chambers potentially influenced by other risk factors. The research shown in the article strongly suggests that combined spatial analysis with geotechnical analysis may lead to reliable sinkhole risk assessment methodology.
Results of reconnaissance survey _Profile TESZ-2021_FINAL_short version.pdfDr. Arzu Javadova
The results of a reconnaissance survey of a seismic profile on Ukraine territory are presented. Experimental studies were carried out with the aim of additional approbation of direct-prospecting methods and improvement of methodological techniques of their application in the exploration process for oil, gas and natural hydrogen, as well as in the study of the deep structural elements of the Earth. The results indicate that it is promising for the detection of HC deposits in the cross-section and the expediency of carrying out prospecting works of a detailed nature within it. In the northern part of the research area, by instrumental measurements a basalt volcanic complex has been localized, which is promising for of natural hydrogen and living water accumulations searching in the cross-section. During the cross-section scanning, responses at gas frequencies were recorded without interruption up to 5 km, which may indicate the presence of a deep channel within the surveyed area, through which oil, condensate and gas migrate to the upper horizons of the cross-section. The results of the survey indicate the advisability of direct-prospecting methods and technologies using when studying the deep structure of small areas and large blocks by geoelectric and seismic methods.
NMR water exploration & presentation of water project technology Fands-llc
The technology will be able to remotely detect and assess groundwater accumulation and flows anywhere on Earth to a depth of 5 km directly.
At a time of deep recession in the global industry and staff reduction, only NMR technology will allow companies to maintain their exploration and prospecting programs scheduled for 2020 at a symbolic price.
( NMR technology provides acquisition of absolute field data with efficiency 2.5-3.0 times higher than indirect seismic data and at a price ten times lower than 2D/3D seismic data).
And most importantly, we are operating remotely, we are not afraid of the coronavirus pandemic all over the world!!!
We will search for reserves and water flows remotely with high accuracy anywhere in the world:
- the identification and contouring of accumulations and flows of underground fresh water,
- mapping the contours;
- obtaining the number of horizons and the depth of their occurrence;
- determining thickness aquifers and reservoir rocks,
- Determination of promising drilling points.
The NMR technology is based on the phenomenon of resonance, which allows direct detection and contouring of accumulations and flows, like the MRI scanning in medicine, which allows seeing human body problems at once.
RESULTS OF THE APPLICATION OF DIRECT-PROSPECTING TECHNOLOGY OF SATELLITE IMAG...Dr. Arzu Javadova
The results of reconnaissance studies within the Shakal and Halabja exploration blocks in Kurdistan are presented. Experimental studies were carried out using a mobile direct-prospecting technology, including modified methods of frequency-resonance processing and decoding of satellite images and photo images, vertical electric resonance scanning of the cross-section and a method of integral assessment of the oil and gas potential of large prospecting blocks and license areas. At the local survey site within the Shakal block, responses from oil, condensate, phosphorus and limestone were recorded. The lower boundary of the limestones was established at a depth of 4676 m. By scanning the cross-section from 2770 m, step 1 cm, the responses of oil from limestones were obtained from the intervals: 1) 2771-2794 m, 2) 2795.3-2815.45 m, 3) 2834.40-2854 m. During processing the image of the entire Halabja block, signals were recorded at the frequencies of oil, condensate, phosphorus gas, bacteria, sodium chloride and dolomite. At the 57 km hydrocarbon synthesis boundary, responses from oil, condensate and gas were recorded. When scanning the cross-section from 480 m to 4 km, step 50 cm, responses from oil were obtained from two intervals: 1) 1140-1200 m, and 2) 3310-3340 m. Within the local fragment of the block by scanning up to 5 km with a step of 1 m responses of oil from salt were recorded from the intervals: 1) 295-350 m, 2) 1190-1260 m, 3) 2015-2320 m). The response intervals within the 1st and 3rd horizons have been refined by scanning with a step of 5 cm. The results of experimental studies show that practical application of direct-prospecting methods and technologies will accelerate and optimize the exploration process for oil and gas.
Within the framework of a new, "substance" (“matter”) paradigm of geophysical research, a "direct" search for a specific physical substance is carried out: gas, oil, gas hydrates, water, ore minerals and rocks (gold, platinum, silver, zinc, uranium, diamonds, kimberlites, etc.). The initial stage in the development of this paradigm can be considered the first research and development on the "direct" methods for oil and gas searching.
Subsurface Determination Of Cavities In Limestone Rock Area By Geoelectric Me...IJERA Editor
Two Dimensional of geoelectric method can be used to find out the conductive formation in the earth surface. The purpose of this research is to give the description about the geological subsurface formation, that the high resistivity value is indicate the potential area of cave and void in the limestone rocks. The dipole dipolegeoelectric method is used in this research with the path of lines is 250 m with 10 m electrode spacing. The total lines is 7 and the azimuth is from east to west. Resistivity method is started with inject the electrical current into the earth by current electrode, then potential difference will arise and measured by potential electrode. Variation value of resistance for each layer rock can calculated by divided potential defference with current value. The existence of the cavity is known by the resistivity value is more than 2500 ohm-m, while the cracks have a resistivity of 1500 to 2500 ohm-m.
The Sinkhole Occurrence Risk Mitigation in Urban Areas for the Historic Salt ...IEREK Press
The present research focuses on the definition of a novel methodology for sinkhole risk assessment above shallow salt mines. The research were carried out on the area above the Wieliczka salt mine, a World Heritage site. The study of vertical stresses on the basis of a theoretical state of rock mass deformation in the area of test chambers was performed. Furthermore, the risk of chamber collapse due to ventricular stress exceeding the limit specified in the zone were calculated based on the arch pressure theory. The final stage of the research consists of spatial analysis that leading to the identification of chambers potentially influenced by other risk factors. The research shown in the article strongly suggests that combined spatial analysis with geotechnical analysis may lead to reliable sinkhole risk assessment methodology.
The Sinkhole Occurrence Risk Mitigation in Urban Areas for the Historic Salt ...IEREK Press
The present research focuses on the definition of a novel methodology for sinkhole risk assessment above shallow salt mines. The research were carried out on the area above the Wieliczka salt mine, a World Heritage site. The study of vertical stresses on the basis of a theoretical state of rock mass deformation in the area of test chambers was performed. Furthermore, the risk of chamber collapse due to ventricular stress exceeding the limit specified in the zone were calculated based on the arch pressure theory. The final stage of the research consists of spatial analysis that leading to the identification of chambers potentially influenced by other risk factors. The research shown in the article strongly suggests that combined spatial analysis with geotechnical analysis may lead to reliable sinkhole risk assessment methodology.
Water Impurity Measurement System using MicrowavesSanket Yavalkar
Microwaves can be used to find water impurities like salinity i.e. hardness, Chlorinity, etc. A simple system (prototype) is being designed and tested in this ppt. for measuring salinity of water. This work is done with the help of by Gov. of India's SAMEER organisation as well as Gov. of Maharashtra's Irrigation Department.
Hydrographic surveying or bathymetric surveying is the survey of physical features present underwater. It is the science of measuring all factors beneath water that affect all the marine activities like dredging, marine constructions, offshore drilling etc.
In this report, I shall discuss the importance and applications of hydrographic surveying, the devices used for the hydrographic survivor, how he uses them, and how do they work.
Geophysical techniques work through applying one of several types of force to the ground, to measure the
resulting energy with use of geophysical equipment and infer the geology from this. Geophysics is generally
much quicker than the aforementioned methods, however, requires more data processing (oìce-based work)
to develop the geological picture. A great advantage of these methods is that certain instruments can be
attached to small aircraft for covering large areas during regional airborne surveys. This provides sparser
geological information, but can highlight potential metal anomalies on a county-country scale, which can be
followed up by more detailed, ground-based geophysical surveys. However, as the material is being tested
indirectly, there is no 100% guarantee of its conclusions; in addition to being susceptible to contamination by
many man-made metallic structures e.g. power-lines. Therefore, should geophysical surveys prove suìciently
interesting, drilling will be required afterwards to conêrm the accuracy of the results.
Determination of Thickness of Aquifer with Vertical Electrical Sounding iosrjce
IOSR Journal of Mechanical and Civil Engineering (IOSR-JMCE) is a double blind peer reviewed International Journal that provides rapid publication (within a month) of articles in all areas of mechanical and civil engineering and its applications. The journal welcomes publications of high quality papers on theoretical developments and practical applications in mechanical and civil engineering. Original research papers, state-of-the-art reviews, and high quality technical notes are invited for publications.
The International Journal of Engineering and Science (The IJES)theijes
The International Journal of Engineering & Science is aimed at providing a platform for researchers, engineers, scientists, or educators to publish their original research results, to exchange new ideas, to disseminate information in innovative designs, engineering experiences and technological skills. It is also the Journal's objective to promote engineering and technology education. All papers submitted to the Journal will be blind peer-reviewed. Only original articles will be published.
The papers for publication in The International Journal of Engineering& Science are selected through rigorous peer reviews to ensure originality, timeliness, relevance, and readability
Research Inventy : International Journal of Engineering and Science is published by the group of young academic and industrial researchers with 12 Issues per year. It is an online as well as print version open access journal that provides rapid publication (monthly) of articles in all areas of the subject such as: civil, mechanical, chemical, electronic and computer engineering as well as production and information technology. The Journal welcomes the submission of manuscripts that meet the general criteria of significance and scientific excellence. Papers will be published by rapid process within 20 days after acceptance and peer review process takes only 7 days. All articles published in Research Inventy will be peer-reviewed.
Groundwater Studies in Abakaliki Using Electrical Resistivity Methodiosrjce
Electrical resistivity survey was carried out to investigate the groundwater potential of Abakaliki
urban, a sedimentary area with the oldest Cretaceous rocks (sandstones and shales) which are of Albian age.
The equipment used for the survey include, ABEM terrameter (SAS, 300C), four electrodes, hammer, four reels
of wires, connecting cords, measuring tapes and global positioning system. The survey was carried out in three
different locations. The field layout employed was the schlumberger array. The result of the survey shows that
the average resistivities are 1337.06m for the first layer, 5914. 34m for the second layer, 1277. 59m for
the third layer, 189. 65m for the fourth layer and 695.78m for the fifth layer with probable lithologic
interpretations as lateritic over-burden for the first layer, ferruginised and highly compact clay stone (dry) for
second layer, fissile dry shale, splintery shale(wet) and saturated and pyritised silty shale (wet) for the other
three layers, respectively. The result indicates that potential groundwater would likely be located in the fourth
layer in the study area.
The International Journal of Engineering & Science is aimed at providing a platform for researchers, engineers, scientists, or educators to publish their original research results, to exchange new ideas, to disseminate information in innovative designs, engineering experiences and technological skills. It is also the Journal's objective to promote engineering and technology education. All papers submitted to the Journal will be blind peer-reviewed. Only original articles will be published.
The papers for publication in The International Journal of Engineering& Science are selected through rigorous peer reviews to ensure originality, timeliness, relevance, and readability.
The South Caspian Basin has many confirmed structures. It includes the offshore continuation of several major anticline trends extending from onshore side. The Umid Babek structure is one of the deepest structures of the Baku archipelago. It is strongly dislocated tectonically and is complicated by mud diapirism. Interpretation of 2D seismic data made it possible to determine the calculations for the area and depth in the Umid and Babek structures. The structures of Shah Deniz and Umid Babek are similar in terms of the history of their structural growth. Umid-Babek occupies the most advantageous position on the path of fluid migration from deep zones of depression and has favourable conditions for the accumulation and preservation of hydrocarbon deposits. U
A.J.On ecology issue of South Caspian Lankaran–Talish–Deniz and Khazar areas.pdfDr. Arzu Javadova
The problems deal with the natural conditions, biota and sediments of the South Caspian
within Lankaran–Talish–Deniz and Khazar offshore areas, as well as anthropogenic impact
on the ecological system of this region were discussed.
Water Impurity Measurement System using MicrowavesSanket Yavalkar
Microwaves can be used to find water impurities like salinity i.e. hardness, Chlorinity, etc. A simple system (prototype) is being designed and tested in this ppt. for measuring salinity of water. This work is done with the help of by Gov. of India's SAMEER organisation as well as Gov. of Maharashtra's Irrigation Department.
Hydrographic surveying or bathymetric surveying is the survey of physical features present underwater. It is the science of measuring all factors beneath water that affect all the marine activities like dredging, marine constructions, offshore drilling etc.
In this report, I shall discuss the importance and applications of hydrographic surveying, the devices used for the hydrographic survivor, how he uses them, and how do they work.
Geophysical techniques work through applying one of several types of force to the ground, to measure the
resulting energy with use of geophysical equipment and infer the geology from this. Geophysics is generally
much quicker than the aforementioned methods, however, requires more data processing (oìce-based work)
to develop the geological picture. A great advantage of these methods is that certain instruments can be
attached to small aircraft for covering large areas during regional airborne surveys. This provides sparser
geological information, but can highlight potential metal anomalies on a county-country scale, which can be
followed up by more detailed, ground-based geophysical surveys. However, as the material is being tested
indirectly, there is no 100% guarantee of its conclusions; in addition to being susceptible to contamination by
many man-made metallic structures e.g. power-lines. Therefore, should geophysical surveys prove suìciently
interesting, drilling will be required afterwards to conêrm the accuracy of the results.
Determination of Thickness of Aquifer with Vertical Electrical Sounding iosrjce
IOSR Journal of Mechanical and Civil Engineering (IOSR-JMCE) is a double blind peer reviewed International Journal that provides rapid publication (within a month) of articles in all areas of mechanical and civil engineering and its applications. The journal welcomes publications of high quality papers on theoretical developments and practical applications in mechanical and civil engineering. Original research papers, state-of-the-art reviews, and high quality technical notes are invited for publications.
The International Journal of Engineering and Science (The IJES)theijes
The International Journal of Engineering & Science is aimed at providing a platform for researchers, engineers, scientists, or educators to publish their original research results, to exchange new ideas, to disseminate information in innovative designs, engineering experiences and technological skills. It is also the Journal's objective to promote engineering and technology education. All papers submitted to the Journal will be blind peer-reviewed. Only original articles will be published.
The papers for publication in The International Journal of Engineering& Science are selected through rigorous peer reviews to ensure originality, timeliness, relevance, and readability
Research Inventy : International Journal of Engineering and Science is published by the group of young academic and industrial researchers with 12 Issues per year. It is an online as well as print version open access journal that provides rapid publication (monthly) of articles in all areas of the subject such as: civil, mechanical, chemical, electronic and computer engineering as well as production and information technology. The Journal welcomes the submission of manuscripts that meet the general criteria of significance and scientific excellence. Papers will be published by rapid process within 20 days after acceptance and peer review process takes only 7 days. All articles published in Research Inventy will be peer-reviewed.
Groundwater Studies in Abakaliki Using Electrical Resistivity Methodiosrjce
Electrical resistivity survey was carried out to investigate the groundwater potential of Abakaliki
urban, a sedimentary area with the oldest Cretaceous rocks (sandstones and shales) which are of Albian age.
The equipment used for the survey include, ABEM terrameter (SAS, 300C), four electrodes, hammer, four reels
of wires, connecting cords, measuring tapes and global positioning system. The survey was carried out in three
different locations. The field layout employed was the schlumberger array. The result of the survey shows that
the average resistivities are 1337.06m for the first layer, 5914. 34m for the second layer, 1277. 59m for
the third layer, 189. 65m for the fourth layer and 695.78m for the fifth layer with probable lithologic
interpretations as lateritic over-burden for the first layer, ferruginised and highly compact clay stone (dry) for
second layer, fissile dry shale, splintery shale(wet) and saturated and pyritised silty shale (wet) for the other
three layers, respectively. The result indicates that potential groundwater would likely be located in the fourth
layer in the study area.
The International Journal of Engineering & Science is aimed at providing a platform for researchers, engineers, scientists, or educators to publish their original research results, to exchange new ideas, to disseminate information in innovative designs, engineering experiences and technological skills. It is also the Journal's objective to promote engineering and technology education. All papers submitted to the Journal will be blind peer-reviewed. Only original articles will be published.
The papers for publication in The International Journal of Engineering& Science are selected through rigorous peer reviews to ensure originality, timeliness, relevance, and readability.
The South Caspian Basin has many confirmed structures. It includes the offshore continuation of several major anticline trends extending from onshore side. The Umid Babek structure is one of the deepest structures of the Baku archipelago. It is strongly dislocated tectonically and is complicated by mud diapirism. Interpretation of 2D seismic data made it possible to determine the calculations for the area and depth in the Umid and Babek structures. The structures of Shah Deniz and Umid Babek are similar in terms of the history of their structural growth. Umid-Babek occupies the most advantageous position on the path of fluid migration from deep zones of depression and has favourable conditions for the accumulation and preservation of hydrocarbon deposits. U
A.J.On ecology issue of South Caspian Lankaran–Talish–Deniz and Khazar areas.pdfDr. Arzu Javadova
The problems deal with the natural conditions, biota and sediments of the South Caspian
within Lankaran–Talish–Deniz and Khazar offshore areas, as well as anthropogenic impact
on the ecological system of this region were discussed.
Taxonomic harmonization of Paratethyan brackish ostracods described by Livent...Dr. Arzu Javadova
Neogene ostracods from Paratethys are, potentially, a powerful biostratigraphic tool to depict the geological history of different basins [Styrian, Vienna, Pannonian, Dacian, Euxinic (former extent of the modern Black Sea basin), and Caspian-Aralic basins]. Yet, most species were described by different authors (Reuss, Méhes, Zalănyi, Livental) in mid-19th and early 20th centuries and, often, descriptions and illustrations are very poor. Very likely, the Neogene Paratethyan biodiversity is overestimated due to lack of literature exchange at time or the undervaluation of ecophenotypical intra-specific variability. As a consequence, often, under different specific (or even generic) names could be hidden the same species. Unfortunately, most of the historical ostracod collection are gone lost or destroyed and the only way to solve this problem is to get new samples from the type localities.
Recently, clays and silts cropping out at Babazanan (Azerbaijan), type locality of the species described by Livental in 1929, were re-sampled, and here we present the results of our taxonomical studies of the collected ostracods providing new definition of the specific characters, mainly based on SEM illustration. An updated synonymy, paleogeographic and stratigraphic distribution starting from the extant literature, will be also provided.
Microfauna of the Miocene Deposits in South Caspian_final versionof PRESENTAT...Dr. Arzu Javadova
Comprehensive geological, geophysical study, and exploration drilling resulted in the vast material that makes it possible to assess microfauna content of South Caspian Basin.
Commercial reservoirs have been established in the Miocene in the South Caspian Basin. The Miocene deposits in South Caspian Basin are of great practical and scientific interest as they underlie the formations of the thick Pliocene Productive series. The core samples taken from exploration wells of the Miocene deposits, where were recovered otholitite, abundant ostracod and foraminifera fauna. The studied sections allowed to define the detailed stratigraphy sequences into individual stratigraphic units: Pontian, Sarmatian, Conkian-Karaganian, Chokrakian, Maikopian deposits
The facies of the Miocene deposits in the South Caspian offshore part of Basin vary considerably and these different facial sedimentary environments affected the microfauna composition as well. This is confirmed by rather abrupt changes in microfauna features from different regions of South Caspian Basin. The Miocene deposits of South Caspian offshore part of basin is rich in microfauna and many of ostracod species here were common in the Tethys and Paratethys bioprovince and is known as brackish and shallow marine genus in the ecology of ostracod assemblages
Javadova Dr.A. Geological and geophysical assessment of the south caspian off...Dr. Arzu Javadova
For the geological and geophysical assessment of the South Caspian offshore Kapaz structure, seismic data were used with the construction of several structural maps. Four seismic horizons have been mapped: the top Pereriva, top Balakhany, top Surakhany suits, and top Akchagyl stage. The results of three wells drilled in the past were analyzed, the well- logs were correlated with neighboring exploration wells.
Interpretation of seismic data shows that the Kapaz structure is located on the border of the sedimentary sources of the paleo Volga and paleo Amudarya. Regional seismic indicates that the paleo Volga probably continued to be the main source of terrigenous deposits. However, the Paleo-Amu Darya became a more important source of sediments during the Apsheron time. This is evidenced by the presence of clinoforms in seismic profiles direction, which is shown from the shelf margin in the dip direction to the west and southwest direction. It is shown that the Paleo-Amu Darya system eventually overlapped and pushed on the margin of the paleo-Volga shelf, effectively sealing the underlying terrigenous reservoir rocks. Growing diapir folds and compartmentation (southern and northern flank) were also observed in the feature of the structure. The reserves' calculation was carried out for each block of the Kapaz structure in scenarios P90, P50 and P10
Прямопоисковая мобильная технология разведки на русском.pptDr. Arzu Javadova
В рамках новой, «вещественной» парадигмы геофизических исследований осуществляется «прямой» поиск конкретного физического вещества: газа, нефти, газогидратов, воды, рудных полезных ископаемых и горных пород (золота, платина, серебро, цинк, уран, алмазы, кимберлиты и др.).
A.j.on ecology issue of south caspian lankaran–talish–deniz and khazar areasDr. Arzu Javadova
Thus, the analysis of the borehole data, seismic data, and biostratigraphy confirmed that the Tertiary sediments consist of fluvial- deltaic–lacustrine sediments deposited in the isolated South Caspian Basin, particularly in the study area by several river systems.
The study area has several characteristics typical of landlocked marine environments: Low salinity; low HD conditions, causing stratification of the water column. High primary productivity of the water mass, generating conditions of dissolved oxygen supersaturation and deficits (of phosphorus and probably of oxygen at night). Also at the sediment level, the heterogeneity of the substrate and low benthic fauna content is typical of confined habitats, in which environmental conditions are especially difficult for the higher organisms.
The micro-pollutant concentration in both the water and sediment, a point also common to most confined habitats and related to the inflow from the catchment area. It is related to the fine fraction of the sediment and may be masked by the presence of numerous shell debris which “dilute” the muds and thereby the micro-pollutants and organic matter, usually settled on these fine sediment fractions. All the observations made on the study, substantial primary production, a paucity of benthos, etc are consistent with those made by different authors describing the Caspian Sea. The study area has high quantities of contaminants and low capabilities for dispersing potential intake, but on the other hand, has a distinct resistance to the influence of any future impediments
Geological & Prospective peculiarity of Kapaz field on South Caspian basin,Dr. Arzu Javadova
Kapaz field is located in the central part of the Apsheron-Pribalkhan threshold between the Azeri and Livano structures- in the west of the Caspian sea. Water depth changes from 90 m in the east to 130 m in the west, in the area. In the seismic cross-sections of the Kapaz field, deposits from Quaternary to Miocene are observed, the cross-sections were revised using the Ostracoda and Formaninifera fauna contents based on regional well correlations. The tectonic structures are an asymmetric anticline striking NW-SE. The folding undulated the upper Pliocene twice and the middle Pliocene thrice. Secondary undulations present as dome-shaped uplifts (3-5 1.5-2,0 km). The size on the fold in the base of the upper division of the middle Pliocene is 25 x2.5 km. The structure in the base of the upper division of the Middle Pliocene is displaced relative to the structure of the top of the mIddle Pliocene to the northwest along the fol axis 3.5-4 km. Oil and gas potential in the southwestern and northeastern slopes of the structure is associated with the deposits from the suite of Pereriva and also with the underlying suits of PS. Concerning Kapaz field evaluation, it is recommended to drill wells to strip up to the KaS as it was done in the Turkmenistan sector of the Caspian Sea in the Livanova, Gubkina, and Lam field. Taking into account the anomalous high-pressure layer below the suite of Pereriva every effort should be taken to strip up to the KaS successfully
To the geology of tertiary quaternary sediments of south-west part of the ...Dr. Arzu Javadova
The SW part of south Caspian offshore studied very poorly. Data studied from numerous offshore shallow engineering and deep exploration wells have provided useful information on the geology of the Tertiary- Quaternary sediments. The log, seismic data, and biostratigraphy confirmed that the Tertiary sediments consist of fluvial- deltaic–lacustrine sediments deposited in the isolated South Caspian Basin, particularly in the study area by several river systems. A Quarternary period is characterized by brackish water sediments. The "short" series of marine sediments of the deep and shallow facies of open sea bays, delta, and marine shallow waters are typical for the SW part of the Caspian.
Pliocene and Quaternary sediments unconformably overlie more ancient formations, until the Mesozoic sediments are located at a relatively shallow depth. In the Lankaran-Talysh Deniz, the Miocene sequences below the middle part of Pliocene Pereryva formation are pinching out against the basin margin. The thickness of these series increases stepwise across the main structures giving evidence of a rift-system developing at the beginning of major subsidence in the South Caspian during the early Tertiary. No hydrocarbon discovery except little oil and gas shows are found in SW of the Caspian due to several geological reasons such as a reservoir, vertical and lateral migration problem.
STRATIGRAPHIC PECULARITIES OF OSTRACOD DISTRIBUTION IN BAKU ARCHIPELAGO, THE ...Dr. Arzu Javadova
Poster presentation for Kazan russian conference.24 29.09.2018
Нами были изучены остракоды из пробуренных скважин северного и центрального Бакинского архипелага: Бахар, Бахар-2, Шах дениз, Аран дениз, Себаил, Ленкоран дениз, Курдаши, Инам, Песчаний и др. Каспийского моря, что позволило коррелировать состав остракодовой фауны четвертичных отложений (рис. 1). В нашем распоряжении было свыше 350 образцов, около 100 видов Leptocythere и Loxoconcha. В целом, выделенный нами состав остракод Южного Каспия позволяет расчленить четвертичные отложения на новокаспийский, хвалынский, хазарский, бакинский и апшеронский надгоризонты с соответствующими горизонтами и слоями (рис. 2). Характерный комплекс постплиоценовой фауны остракод хорошо коррелируется с прибрежными разрезами Апшеронского полуострова: Песчаный, Алят, Локбатан, Пирсагат, Нефтчала. При определении видового состава использовались СЭМ фотографии остракод, собранных нами из скважин Апшеронского и Бакинского архипелагов
his paper presents the Microbial Prospection for Oil and Gas (MPOG) method, which uses microbiological techniques to explore for oil and gas. These techniques are based on the principle that light hydrocarbons from oil and gas fields escape to the earth’s surface, and this increased hydrocarbon supply above the fields creates conditions favorable for the development of highly specialized bacterial populations that feed on the hydrocarbons. This leads to significant increases in the microbial cell numbers and cell activity of these specialized microbes. By developing methods to establish the separate activities of methane-oxidizing bacteria (a gas indicator) and those bacteria that oxidize only ethane and higher hydrocarbons (oil indicators), it is possible to differentiate between oil fields with and without a free gas cap, and gas fields.In unexplored areas, MPOG represents a cost-effective method for preliminary exploration work. In mature areas, the method is helpful for ranking seismically defined geologic structures by indicating possible infill locations, as a contribution to reservoir characterization. No geologic or seismic data are required to carry out microbial prospection. In areas that have not yet been investigated geophysically, this technique can be applied as wildcat prospection. The sampling points are laid over the surface to be investigated, in the form of a map grid. The biochemical activity of the HCO represents the cumulative parameters. These are calculated by
• quantifying the consumption of added hydrocarbons (methane and/or propane and butane) using gas chromatography and pressure measurements • determining the biological CO2 formation rate
Microbial enhanced oil recovery (MEOR) represents the use of microorganisms
to extract the remaining oil from reservoirs. This technique has the potential
to be cost-efficient in the extraction of oil remained trapped in capillary pores of
the formation rock or in areas not swept by the classical or modern enhanced oil
recovery (EOR) methods, such as combustion, steams, miscible displacement, caustic
surfactant-polymers flooding, etc. Thus, MEOR was developed as an alternative
method for the secondary and tertiary extraction of oil from reservoirs,
The Quaternary deposits of the South Caspian and the adjacent areas on ostrac...Dr. Arzu Javadova
The South Caspian is one of the largest oil-producing regions within the Caspian Sea. Most of the offshore fields are focused here along with the main geologic oil and gas reserves of Azerbaijan. The development of the discovered fields, prospects and exploration of new ones require detailed study of the Quaternary deposits: their material composition, stratigraphy, thicknesses and other properties. It is necessary to study these issues not only for improvement of the efficiency, provide safe geological prospecting and exploration, but also to solve engineering and geological tasks related to the planned development of discovered oil and gas fields.
Study of fauna and stratigraphy of the Quaternary deposits in the South Caspian is important to learn the Quaternary history of the Caspian Sea. The Quaternary time is known for its frequent and abrupt fluctuations in climate, ocean and sea levels, considerable changes in topography, fauna, flora and other natural components of the Earth. The large-scale well drilling in the South Caspian water area provided geological information particularly about ostracod fauna, stratigraphy and litho-facies features of the Quaternary deposits of the studied regions.
We investigated the systematic composition and distribution regularities of ostracod fauna from the Quaternary deposits over the vast South Caspian territory, including the stratigraphic role of the fauna and correlation of the data with the coastal –onshore area. Multiple well sections and their enclosed micro- and macro fauna were the study target. When we analyzed and correlated well sections and natural outcrops we used other methods like lithological, macro fauna, radiometric, electric logging, seismic logging as well. The result of our study allowed us to design a detailed stratigraphic chart for the Quaternary deposits of the entire South Caspian basin. For the first time the Quaternary deposits of the South Caspian breakdown with 5 supra horizons, 10 horizons with 7 index species. Index species were identified on the successive change of zonal complexes- biozones. All these subdivisions play a regional role and correlated well with the ones from the adjacent areas of the Caspian region.
The paleontological processing of individual ostracod of genera: Leptocythere, Amniocythere, Euxinocythere, others allowed us to identify specific features among them in order to differentiate a new ostracod species.
We also highlighted the issues of stratigraphy, facies analysis and thicknesses of the Quaternary deposits in the South Caspian. The analysis of facies, thicknesses and fauna distribution shows that in the Quaternary time the South Caspian region was characterized by rather dynamic paleogeographic settings: along with the active change of the sea bottom topography, salinity and temperature varied considerably and often, as well as the sea level.
Geological &prospective peculiarity of Kapaz field on S.Caspian part 29 36Dr. Arzu Javadova
This presentation published in international Earth Sciences Colloquium of the Aegean Regions, in Izmir, Turkey in 2005. The Apsheron trend characterised by large, east to west striking folds and structures of the Pliocene section overlying and burying the underlying rifted margin structures and half-grabens of the Cretaceous, Jurassic and possibly Triassic continental margin and shelf. The Tertiary structures display strike-slip influence, such as reversal of normal faults that bound the underlying half grabens; local back thrusting and flower-like structuring are common. The most significant volumetric potential lies in the offshore. Three elements are key to the extraordinary oil and gas potential of the South Caspian Basin. The high-quality reservoir sands are the Volga Pliocene delta and a lesser extent.
Geological &prospective peculiarity of Kapaz field on S.Caspian part 19 27Dr. Arzu Javadova
This presentation published in international Earth Sciences Colloquium of the Aegean Regions, in Izmir, Turkey in 2005.S.Caspian basin is prominent basin with thick MZ-GZ terrigenous depositional fill encompassed by Alpine fold belt. The S. Caspian deep and basin proper is probably remnant oceanic crust of the Neo Thethys caught (пойманный) between the Jurassic Сretaceous carbonate platform and continental margin in the north accreted islands arc terrаin and Gondwana in the south.
S. Capsian basin borders with prominent folt system of Major Caucasus & Copetdag on the north which are linked together across the basin via Apsheron-Pre Balkhan uplift belt which consists of 2 anticline lines: Apsheron-Turkmenbashy and Apsheron-Cheleken one
LF Energy Webinar: Electrical Grid Modelling and Simulation Through PowSyBl -...DanBrown980551
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- A fully editable and extendable library for grid component modelling;
- Visualization tools to display your network;
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In the rapidly evolving landscape of technologies, XML continues to play a vital role in structuring, storing, and transporting data across diverse systems. The recent advancements in artificial intelligence (AI) present new methodologies for enhancing XML development workflows, introducing efficiency, automation, and intelligent capabilities. This presentation will outline the scope and perspective of utilizing AI in XML development. The potential benefits and the possible pitfalls will be highlighted, providing a balanced view of the subject.
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Alt. GDG Cloud Southlake #33: Boule & Rebala: Effective AppSec in SDLC using ...James Anderson
Effective Application Security in Software Delivery lifecycle using Deployment Firewall and DBOM
The modern software delivery process (or the CI/CD process) includes many tools, distributed teams, open-source code, and cloud platforms. Constant focus on speed to release software to market, along with the traditional slow and manual security checks has caused gaps in continuous security as an important piece in the software supply chain. Today organizations feel more susceptible to external and internal cyber threats due to the vast attack surface in their applications supply chain and the lack of end-to-end governance and risk management.
The software team must secure its software delivery process to avoid vulnerability and security breaches. This needs to be achieved with existing tool chains and without extensive rework of the delivery processes. This talk will present strategies and techniques for providing visibility into the true risk of the existing vulnerabilities, preventing the introduction of security issues in the software, resolving vulnerabilities in production environments quickly, and capturing the deployment bill of materials (DBOM).
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Bob Boule
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Enchancing adoption of Open Source Libraries. A case study on Albumentations.AIVladimir Iglovikov, Ph.D.
Presented by Vladimir Iglovikov:
- https://www.linkedin.com/in/iglovikov/
- https://x.com/viglovikov
- https://www.instagram.com/ternaus/
This presentation delves into the journey of Albumentations.ai, a highly successful open-source library for data augmentation.
Created out of a necessity for superior performance in Kaggle competitions, Albumentations has grown to become a widely used tool among data scientists and machine learning practitioners.
This case study covers various aspects, including:
People: The contributors and community that have supported Albumentations.
Metrics: The success indicators such as downloads, daily active users, GitHub stars, and financial contributions.
Challenges: The hurdles in monetizing open-source projects and measuring user engagement.
Development Practices: Best practices for creating, maintaining, and scaling open-source libraries, including code hygiene, CI/CD, and fast iteration.
Community Building: Strategies for making adoption easy, iterating quickly, and fostering a vibrant, engaged community.
Marketing: Both online and offline marketing tactics, focusing on real, impactful interactions and collaborations.
Mental Health: Maintaining balance and not feeling pressured by user demands.
Key insights include the importance of automation, making the adoption process seamless, and leveraging offline interactions for marketing. The presentation also emphasizes the need for continuous small improvements and building a friendly, inclusive community that contributes to the project's growth.
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Explore more about Albumentations and join the community at:
GitHub: https://github.com/albumentations-team/albumentations
Website: https://albumentations.ai/
LinkedIn: https://www.linkedin.com/company/100504475
Twitter: https://x.com/albumentations
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- Improved developer experience and productivity through actionable findings and reduction of false positives
- Maintenance of superior security standards and inherent policy enforcement with Authorization to Operate (ATO)
Development teams can ship efficiently and ensure applications are cyber ready for Navy Authorizing Officials (AOs). In this webinar, Sigma Defense and Anchore will give attendees a look behind the scenes and demo secure pipeline automation and security artifacts that speed up application ATO and time to production.
We will cover:
- How to remove silos in DevSecOps
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- How to streamline operations with automated policy checks on container images
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Goodbye Windows 11: Make Way for Nitrux Linux 3.5.0!
Presentation1 final shortened.pdf
1. WMESS- 2021, Prague, Czech Republic,
APPLICATION OF FREQUENCY-RESONANCE METHODS OF
SATELLITE IMAGES PROCESSING FOR HYDROGEN AND
LIVING WATER ACCUMULATIONS SEARCHING WITHIN
LOCAL AREAS IN EUROPE
Yakymchuk N.A.1, Korchagin I.N.2, Javadova A.3
1Institute for Applied Problems of Ecology, Geophysics and Geochemistry, Laboratory Lane, 1, Kyiv, 01133,
Ukraine, e-mail: yakymchuk@gmail.com
2S.I. Subbotin Institute of Geophysics of the NAS of Ukraine, Palladin Ave., 32, Kyiv, 03680, Ukraine, e-mail:
korchagin.i.n@gmail.com
3MikroPro GMBH, st. Magdeburg 26, b, Gommern, 39245, Germany, e-mail: javadova@micropro.de
1
2. Current situation with the production of Hydrogen
• Problem with the production of hydrogen not yet resolved. The world, does not allow large-scale research for
prospecting and exploration of reserves natural hydrogen. No active search for natural sources of hydrogen
• A natural hydrogen well Bugu-1 provides electricity to a village in Mali. But it is surprising that no one further
studied the deposit. Therefore, until now, the source of hydrogen has not been established there.
• A similar situation in the world was relatively recently with methane. The target product of geological
exploration was oil, and the natural gas fields discovered during geological exploration were simply preserved.
Without any further research. As a result, even now, many regions of the world have been extremely poorly
studied for the presence of methane in their bowels.
• The concept of "initially hydride Earth", according to which the key role in the evolution of the planet is playing
hydrogen. , in the earth's crust it does not contain a fraction of a percent, as was previously thought, and
about 60% by volume and 5% by weight. That is the Earth supersaturated with hydrogen. It is released from
the core of the planet through the earth's crust into the atmosphere, where its constant concentration is kept
at the level of 2.5 million tons. Moreover, in the process of such "hydrogen degassing" of the order of 250
thousand tons of hydrogen goes into space annually.
2
3. Introduction
• In 2019-2021 in various regions of the world, a
large amount of experimental research has been
carried out with the aim of testing frequency-
resonance methods of satellite images and photo
images processing and decoding,
• In the course of the work, the possibility of
purposeful application of mobile direct-
prospecting technology was additionally studied
for hydrogen accumulations detecting in areas of
hydrogen degassing and determining the depths
(intervals) of their occurrence.
• Some results of the experimental investigation in
order to study the possibility of direct-prospecting
methods using for localizing hydrogen
accumulations in the cross-section are given in
EAGE conference 2019
а) б)
в) г)
д) е)
Figure 1 Satellite images of local areas on the
territory of Azerbaijan. Rectangular contours
indicate fragments of frequency-resonance
processing
3
4. Our biggest mistake is not listening in
order to understand. We listen to
answer.
Omar Khayyam and other great
philosophers
Figure 2. Model (fragment) of the Earth's crust: h1 – h3 - thickness of sedimentary rock strata;
1–3 - their dielectric constant;
1-3 - the boundaries of the layers; I – III - antinode of standing waves
I can never forget the first sensations that I experienced when it dawned on my mind that I was watching
something that might have unpredictable consequences for humanity. I felt myself present at the birth of
a new knowledge or at the discovery of a great truth. Nicola Tesla
The developed methods are
based on the standing electric
waves discovered by Nikola
Tesla in 1899
Earth surface
Method
4
5. Remote Sensing
data processing and
interpretation
Forming a Short-Pulsed
Electromagnetic Field
Vertical Electro-
Resonance Sounding
The technology consists of three innovative methods based on
the frequency-resonate concept:
The development of technology took place at the forefront of two
sciences: GEOPHYSICS AND ATMOSPHERIC PHYSICS
Remote Sensing data processing
and interpretation
Fixing pulsed natural
electromagnetic fields of the Earth’s,
it is possible to study also it effects
satellite images of the Earth's
surface in different spectral
channels.
Current development of computer
technology does not allow for the
spectral analysis of all possible
channels recorded by satellites,
where there is also information on
the structure of the Earth and the
objects in it.
To solve this problem author has
used an analog optical processing
method by which it became
possible to carry out the
classification of satellite images and
allocate them abnormal radiation
from various geological bodies in
their frequencies. 5
6. Figure 3 Measuring equipment: on the long line
generator (LLG) (aluminum box) there are three
modifications of the fluxmeter
Figure 4 Sets of frequency resonance
sounding equipment to a depth of 118
km (left) and 25 km (right).
The shown hardware measuring systems have been tested during research at the Ukrainian marine Antarctic Expedition of 2018
Measuring equipment
6
7. Results of instrumental measurements in Latvia and Lithuania
different region
Figure 5. Latvia.
A satellite image of the site
in the area of well drilling
for hydrogen in Latvia. The
drilling location is indicated
by a red marker
Figure 6. Satellite image of
the survey site in Lithuania.
Signals were recorded at
the frequencies of :
depth
scanning the cross-
section with a
step of 10 cm
hydrogen 28 m
the 6th (basalt) group of
igneous rocks
volcano filled with basalts 470 km
the upper edge of
the basalts was
determined at a
depth of 26 m
hydrogen from surface 140-235 m
phosphorus (white) from surface
deep (living) water from surface 317 m
sedimentary rocks of the
9th group (marls) from surface 254 m
igneous rocks of the 6th
group (basalts from surface
The root of the basalt
volcano was identified at
a depth of: 470 km
the upper edge of the
basalts was recorded at
an elevation of: 254 m
Figure 1
Figure 2
Latvia
Lithuania
7
8. Results of instrumental measurements in Ukraina
Figure 7 Satellite image of survey sites in the area of Lake
Chervone (lower right rectangle).
Signals were
recorded at the
frequencies of :
depth
scanning the cross-section
with a step of 10 cm
The lower edge
of basalts was
determined at:
98 k m
the upper edge
was established
by scanning at a
depth of :
100 m
10th group of
sedimentary
(siliceous) rocks
were recorded
on the surface
of:
99 km
the root of the
volcano of these
rocks was
determined at:
723 km
Hydrogen
0 m. migration
into the
atmosphere
By scanning the cross-
section from 80 m, step 10
cm, signals from hydrogen
began to be recorded from
100 m
deep water 112 m
Signals from
dead water were
received at:
71
basalts
By scanning the cross-
section from the surface,
step 1 m recorded from
1010 m and traced to 99
km
The 10th group
of sedimentary
(siliceous) rocks
were obtained
from the lower
part of cross-
section.
On the surface
of 99 km
By fixing the
responses at
different depths
(150, 250, 450,
550, 650, 750,
723 km),
the root of the
volcano with
siliceous rocks
was identified
at a depth of
723 km
1-6 groups of
sedimentary
rocks, oil,
condensate,
amber, carbon
dioxide,
phosphorus
On the surface
of 1010 m
hydrogen were
recorded from
1165 m and
traced to 2 km
By scanning the section
from 1000 m, step 50 cm
carbon dioxide 0
responses from
hydrogen and
phosphorus
absent
deep (living)
water began to
be recorded from
By scanning the cross-
section from 1000 m, step
1 m, 1320 m
hydrogen-rich
water
Additional
examination
of the interval
Figure 3
Figure 7
8
9. Results of instrumental measurements in Poland
Figure 8. Satellite images of survey sites in Poland.
a) b)
Signals were
recorded at the
frequencies of :
depth
scanning the
cross-section
with a step of 10
cm
8th (dolomites), 470 km
9th (marls) ,The
root of the volcano
of marls
98 km
The root of the
volcano of 10th
(siliceous) groups
723 km
The root of the
volcano of 7th
group of
sedimentary rocks
(limestones)
99-217 km
The root of the
volcano of siliceous
rock
217 km
The root of the
ultramafic rocks
470 km
The root of the
volcano of basalts
was determined at
723 km
the 9th (marl) group
of sedimentary
rocks
218-470 km
the upper edge of
the basalts was
fixed at
107 m
hydrogen and
dolomites
107 m
hydrogen and
dolomites
By scanning the
cross-section
from the surface
to a depth of 107
m, step 5 cm 63-
83 m
hydrogen responses
from basalts began
to be recorded
from of living water
scanning the
cross-section
from a depth of
107 m, a step of
10 cm, 139 m
living water 220 m
Figure 4 a)
Figure 4 b)
Figure 8
9
10. Results of instrumental measurements in Ikaria island (Aegean
Sea, Greece
Figure 9. Satellite image of the Ikaria island (Aegean Sea, Greece
Ikaria Island is the island of centenariansю
Water synthesis occurs at a depth of 68. The basalts volcanoes also contain hydrogen. And
hydrogen-rich water has healing properties and promotes longevity
Signals were recorded at
the frequencies of :
depth
scanning the cross-
section with a step
of 10 cm
hydrogen
1) 89-880 m; 2)
2812-3182 m; 3)
3507- (responses
traced up to 15 km)
water
1) 40-93 m; 2) 110-
400 m (traced only
up to 400 m).
When scanning the cross-
section from 70 m, step 10
cm, responses at hydrogen
frequencies from the 8th
group of sedimentary
rocks (dolomites) were
recorded
1) 89-218 m; 2) 244-
356 m; 3) 418-580
m; 4) 650-664 m; 5)
765-812 m; 6) 836-
848 m; 7) 871-880
m; 8) 887-893 m
responses were obtained
from only one sample of
the 8th group of
sedimentary rocks -
oncolytic dolomite, salt
&sedimentary rocks of 1-3
groups
89-893 m,
the root of basalt volcano
was determined at :
By fixing the
responses from
basalts at different
depths (50, 150,
450, 550, 750, 723
km) 723 km
the upper edge of the
basalts
3-4 km
the 14th group of igneous
rocks, in which there are
samples with the
properties of marls
By scanning cross-
section with a step
of 50 cm, signals
from these rocks
were recorded in
the interval of 160-
260 m
By fixing the responses
from basalts at different
depths (50, 150, 450, 550,
750, 723 km), the root of
basalt volcano was
determined at:
723 km
the 8th group of
sedimentary rocks -
oncolytic dolomite;
sedimentary rocks of 1-3
groups ; salt
89-893 m,
Figure 5
Figure 9
10
11. Results of instrumental measurements in Italy
Figure 10. Satellite images of local areas of
hydrogen degassing in Italy.
Signals were recorded at the
frequencies of :
depth
The lower boundary of the
basalts is determined at:
(rectangle 1 ; 2 &3)
99 km
the 9th group of
sedimentary rocks (marls).
(rectangle 1)
99-470 km
the 8th group of
sedimentary rocks
(dolomites),(rectangle 2) ;
the 8th group of
sedimentary rocks (marls)
(rectangle 3)
99-470 km
(rectangle 2)
99-218
(rectangle 3)
the 10th group of
sedimentary rocks (siliceous
rocks)
218-723 km
Figure 7
Figure 10
11
12. Results of instrumental measurements in UK
a) b)
Signals were recorded
at the frequencies of :
depth
scanning the cross-
section with a step of
10 cm
the root of the volcano
of siliceous rocks
470 km
dolomites and basalts
at 723 km
the upper edge of the
basalts
388 m
responses from
dolomites, as well as
hydrogen from
dolomites
At the surface
(depth) of 388 m
hydrogen from
dolomites
from the surface to a
depth of 388 m, step
10 cm 265-378 m
dolomite 265 m
signals at hydrogen
frequencies began to
be recorded from
basalts from: 410 -500 m
living water 425-508 m
Dead water responses
were recorded at: 71 km
Signals from hydrogen
and phosphorus were
recorded at:
0 m, which indicates
their migration into
the atmosphere
Figure 11. Satellite images of survey sites in the
vicinity of London: Heathrow airport area (a); area
of St. Mary Cray, Orpington (b).
Signals were
recorded at the
frequencies of :
depth
scanning the cross-
section with a step
of 10 cm
The upper edge of
the basalts was
determined by
scanning from 0 m,
step 1 cm at
3.5 m
The root of the
basalt volcano was
recorded at
723 km
responses from
hydrogen began to
be recorded from
9 -100 m
living water 25 m
12
13. a)
b) c)
Results of instrumental measurements in
UK & Scotland
Figure 12. Areas of investigation in England: photograph of
Doune Hill and Moorland in Scotland [2] (a); satellite
image of a well at Preston New Road (Lancashire) (b);
photographs of crop circles in England [5] (c).
The results of frequency-resonance processing of satellite
images and photographs of areas of peat bogs in Rivne
and Chernigov regions in Ukraine showed that they are
all located above basalt volcanoes, in the contours of
which hydrogen migrates into the atmosphere
Drilling site in England. During processing a satellite image of a well
for shale gas location in England (figure 8b), responses from
hydrogen and basalts were also recorded. Signals from basalts were
recorded up to 95 km
Signals were
recorded at the
frequencies of :
depth
scanning the
cross-section
with a step of 10
cm
a volcano filled
with sedimentary
rocks of the 9th
group (marls). The
root of the volcano
was identified at:
723 km
Signals from
basalts were
recorded in
4.8-98000 m.
responses from the
9th group of
sedimentary rocks
(marls)
98-723
km
hydrogen from
basalts began to be
recorded from
6 m
living wate 7.5 m
Peatland site in Scotland
Crop circles in England.
On the surface of 0 m
from the upper part of
cross-section, responses
from hydrogen and
phosphorus were
recorded for all circles,
which indicate of these
elements’ migration into
the atmosphere within
areas of circles location
13
14. Results and discussions
A) In the areas and region of the basalt volcano’s location with roots at different depths, signals at hydrogen frequencies
from the surface are almost always recorded.
B) Responses from hydrogen are recorded when scanning section practically from the upper edges of basaltic
volcanoes to their roots
C) In some types of basalt volcanoes at a depth of 68 km, deep (living) water is synthesized. Hydrogen-rich water is
healing and can be used for wellness purposes. It is advisable to note once again that all surveyed zones and areas of
longevity on Earth are located within (contours) of basalt volcanoes, in which water synthesized at a depth of 68 km
migrates to the surface and is used for water supply and drinking purposes.
D) Hydrogen deposits can be formed by basaltic volcanoes in sealed reservoirs adjacent to basalts. The Mali hydrogen
production site is located outside the contour of the basalt volcano; Hydrogen responses were recorded at the marl well
site. At other survey sites, signals from hydrogen were obtained from dolomites (Carpathians, the island of long-lived
Ikaria), as well as from marls and limestones
E) Hydrogen deposits formed near basalt volcanoes in different types of reservoirs can be operatively discovered and
localized during areal exploration using direct-prospecting methods (technology of frequency-resonance processing of
satellite images and photo images, including).
F) The problem of studying reservoirs in crystalline rocks (basalts including) also deserves attention. Direct-prospecting
methods can also be used for this purpose.
G) The facts of hydrogen migration into the atmosphere within the discovered basalt volcanoes in different regions of
the world, recorded by instrumental measurements, should be considered fundamentally important. In general, the above
research results confirm the conclusions of the researchers about the large-scale migration of deep (abiogenic) gas and
hydrogen into the atmosphere of Earth planet!
14
15. Conclusions
• The materials of experimental research of a reconnaissance nature, presented in
the article, clearly demonstrate the working capacity, information content and
promptness of direct-prospecting methods of satellite images and photo images
frequency-resonance processing during an integrated assessment of the prospects
of hydrogen accumulations detecting within survey areas, as well as in the
intervals of cross-section of local site.
• The results of experimental work in various regions indicate the advisability of
using direct-prospecting methods of satellite images and photographs frequency-
resonance processing and decoding to detect and localize zones of hydrogen
accumulation in areas of basalt volcano’s location, as well as within sites of
hydrogen degassing.
• The use of super-operational and low-cost direct-prospecting technology will
significantly accelerate the exploration process for hydrogen, as well as reduce the
financial costs for its implementation
15
17. Technology components
Remote Sensing data processing and interpretation
Furthermore fixing pulsed natural electromagnetic fields of the Earth’s, it is possible to study also it effects satellite images of
the Earth's surface in different spectral channels.
Current development of computer technology does not allow for the spectral analysis of all possible channels recorded by
satellites, where there is also information on the structure of the Earth and the objects in it.
To solve this problem author has used an analog optical processing method by which it became possible to carry out the
classification of satellite images and allocate them abnormal radiation from various geological bodies in their frequencies.
17
18. Fig. 2. A group of carbonate rocks.
Dolomites
Fig. 3. A group of kimberlites and lamproyites Fig. 4. Photographs of samples of
chemical elements and minerals: a)
diamonds; b) hydrogen; c) carbon; d)
amber; e) coal.
Base of magmatic and metamorphic rocks
1. Group of granites and rhyolites. 29 samples.
2. Group of granodiorites and dacites. 7 samples
3. A group of syenites and trachytes. 18 samples.
4. A group of diorites and andesites. 14 samples.
5. Rocks of the lamprophyre group. 14 samples.
6. Group of gabbro and basalt. 32 samples.
7. The group of no-feldspathic no-feldspathoid ultramafic rocks. 20
samples.
8. Group of feldspathoid syenites and phonolites. 23 samples.
9. Group of feldspathoid gabbroids and basaltoids. 6 samples.
10. A group of no-feldspathic ultramafic and mafic rocks. 10
samples.
11. A group of kimberlites and lamproites. 20 samples.
12. Non-silicate rocks. Group of carbonatites. 8 samples.
13. Metamorphic rocks of the granulite group. 10 samples.
14. Metamorphic rocks of the gneiss group. 26 samples.
15. Metamorphic rocks of the group of crystalline schists. 44
samples.
16. Metamorphic rocks of the group of microcrystalline schists
(phyllites). 11 samples.
17. Metamorphosed rocks of the slate group. 2 samples.
18. Iron ore. 5 samples
18
19. Fig. 1. Photos of samples of
oil and gas condensate
Base of sedimentary rocks.
1. Group of detrital rocks. Psefits.
Monomineralic conglomerates. 22 samples.
2. Group of detrital rocks. Psammites 18
samples.
3. Group of detrital rocks. Alevrits,
argillites, clays. 6 samples.
4. Group of detrital and clay rocks. Clay
rocks. Argillite kaolinite. 6 samples.
5. Group of detrital rocks. Clay rocks.
Kaolinite clays. 10 samples.
6. Sedimentary-volcanoclastic rocks. 9
samples.
7. Group of carbonate rocks. Limestone. 24
samples.
8. Group of carbonate rocks. Dolomites. 11
samples.
9. Group of carbonate rocks. Marls. 10
samples.
10. A group of siliceous rocks. 13 samples.
11. Salt. 3 samples.
19