North and central caspian basin play maps
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The document discusses oil and gas resources in the North and Central Caspian basin located offshore of Kazakhstan. It provides play maps showing the distribution and size of oil and gas resources in the basin separated for different geological periods including Triassic, Permian, Jurassic and Cretaceous time periods. The play maps aid in understanding the hydrocarbon potential of different areas within the basin over geologic time.
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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...
The document is a geological and geophysical assessment of the South Caspian offshore Kapaz structure. It describes using geological and geophysical data to analyze the structure and stratigraphy of the Kapaz oil and gas field located in the South Caspian Sea. The assessment identifies potential hydrocarbon reserves based on seismic data analysis and interpretation of the geological formations in the region.
Results of reconnaissance survey _Profile TESZ-2021_FINAL_short version.pdf
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.
Direct-prospecting methods_Presentation.ppt
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.
Прямопоисковая мобильная технология разведки на русском.ppt
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 areas
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,
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 ...
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.
2d poster about coring procedure
1. Conventional coring involves pulling the drill string out of the hole, attaching a core barrel assembly, and running it back into the hole to retrieve core samples.
2. The core barrel assembly consists of an inner and outer tube. Mud circulation is used before and during coring to clean the inner tube and divert flow to the annulus to prevent damaging the core sample.
3. To start coring, the drill string is pulled, the coring head is attached and run back into the hole, then mud is circulated and a ball is dropped to start cutting cores which enter the inner tube for retrieval.
1st poster example of core analysis program
The document outlines the key steps for designing and managing an effective core analysis program, including appointing a program focal point, reviewing existing core data, designing the testing program with laboratory assistance, selecting a laboratory contractor, and preparing final reports. It also provides examples of specialized core analysis programs for different reservoir lithologies and examples of recommended routine and special core analysis tests for gas and oil reservoirs.
Days 3d porosity , permeability, fluid saturation
Porosity is a key property of reservoir rocks that represents the pore volume as a fraction of bulk volume. It can be measured through laboratory analysis of rock samples or estimated from well logs. Several factors influence porosity, including grain size, sorting, cementation, and compaction. Common techniques to determine porosity include measuring pore volume directly through fluid extraction or injection methods, or calculating it by finding the grain volume and subtracting it from bulk volume. Understanding porosity distribution is important for reservoir characterization and fluid flow modeling.
Day 2 d coring & core analysis and reservoir geology
This document discusses core laboratory processing and analysis techniques. It covers topics such as core receipt and cutting, CT scanning, gamma ray logging, plugging, slabbing, photography, and special handling considerations for difficult rock types like unconsolidated cores, carbonates, and shales. It provides details on various core analysis techniques and recommendations to minimize core damage during handling and transportation.
Core analysis & wellsite core acquisition, handling and transportation
This document provides an overview of coring and core analysis for reservoir characterization. It discusses the objectives of coring to obtain representative rock samples for analysis. Proper core handling and analysis can provide valuable data on lithology, porosity, permeability, and fluid saturations which help reduce uncertainty in reservoir models. The document outlines procedures for wellsite core handling, transportation, and preservation to minimize alteration. It also discusses conventional and wireline-retrievable coring systems.
South Caspian shallow water Apsheron rend Geology
The document discusses the geology of the Apsheron Trend in Azerbaijan, including its stratigraphy, tectonics, and facies distribution. The Apsheron Trend contains two anticlinal zones - Apsheron-Krasnovodsk and Apsheron-Cheleken - divided by the Kusar-Kelkorian synclinorium. Local structures formed during the Pliocene-Quaternary and were influenced by faults and basement block movement. Source rocks included terrestrial deposits to the north and deposits from the Greater and Lesser Caucasus, supplied by paleorivers. Deposits within the trend contain oil and gas in Pliocene deltaic and coastal marine sands. Structural evolution
STRATIGRAPHIC PECULARITIES OF OSTRACOD DISTRIBUTION IN BAKU ARCHIPELAGO, THE ...
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
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RESULTS OF THE APPLICATION OF DIRECT-PROSPECTING TECHNOLOGY OF SATELLITE IMAG...
RESULTS OF THE APPLICATION OF DIRECT-PROSPECTING TECHNOLOGY OF SATELLITE IMAG...
A.J.On ecology issue of South Caspian Lankaran–Talish–Deniz and Khazar areas.pdf
A.J.On ecology issue of South Caspian Lankaran–Talish–Deniz and Khazar areas.pdf
Taxonomic harmonization of Paratethyan brackish ostracods described by Livent...
Taxonomic harmonization of Paratethyan brackish ostracods described by Livent...
Microfauna of the Miocene Deposits in South Caspian_final versionof PRESENTAT...
Microfauna of the Miocene Deposits in South Caspian_final versionof PRESENTAT...
Javadova Dr.A. Geological and geophysical assessment of the south caspian off...
Javadova Dr.A. Geological and geophysical assessment of the south caspian off...
Results of reconnaissance survey _Profile TESZ-2021_FINAL_short version.pdf
Results of reconnaissance survey _Profile TESZ-2021_FINAL_short version.pdf
Прямопоисковая мобильная технология разведки на русском.ppt
Прямопоисковая мобильная технология разведки на русском.ppt
A.j.on ecology issue of south caspian lankaran–talish–deniz and khazar areas
A.j.on ecology issue of south caspian lankaran–talish–deniz and khazar areas
Geological & Prospective peculiarity of Kapaz field on South Caspian basin,
Geological & Prospective peculiarity of Kapaz field on South Caspian basin,
To the geology of tertiary quaternary sediments of south-west part of the ...
To the geology of tertiary quaternary sediments of south-west part of the ...
Day 2 d coring & core analysis and reservoir geology
Day 2 d coring & core analysis and reservoir geology
Core analysis & wellsite core acquisition, handling and transportation
Core analysis & wellsite core acquisition, handling and transportation
STRATIGRAPHIC PECULARITIES OF OSTRACOD DISTRIBUTION IN BAKU ARCHIPELAGO, THE ...
STRATIGRAPHIC PECULARITIES OF OSTRACOD DISTRIBUTION IN BAKU ARCHIPELAGO, THE ...
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Neutralizing antibodies, pivotal in immune defense, specifically bind and inhibit viral pathogens, thereby playing a crucial role in protecting against and mitigating infectious diseases. In this slide, we will introduce what antibodies and neutralizing antibodies are, the production and regulation of neutralizing antibodies, their mechanisms of action, classification and applications, as well as the challenges they face.
快速办理(UAM毕业证书)马德里自治大学毕业证学位证一模一样
学校原件一模一样【微信：741003700 】《(UAM毕业证书)马德里自治大学毕业证学位证》【微信：741003700 】学位证，留信认证（真实可查，永久存档）原件一模一样纸张工艺/offer、雅思、外壳等材料/诚信可靠,可直接看成品样本，帮您解决无法毕业带来的各种难题！外壳，原版制作，诚信可靠，可直接看成品样本。行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备。十五年致力于帮助留学生解决难题，包您满意。
本公司拥有海外各大学样板无数，能完美还原。
1:1完美还原海外各大学毕业材料上的工艺：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。文字图案浮雕、激光镭射、紫外荧光、温感、复印防伪等防伪工艺。材料咨询办理、认证咨询办理请加学历顾问Q/微741003700
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Signatures of wave erosion in Titan’s coasts
The shorelines of Titan’s hydrocarbon seas trace flooded erosional landforms such as river valleys; however, it isunclear whether coastal erosion has subsequently altered these shorelines. Spacecraft observations and theo-retical models suggest that wind may cause waves to form on Titan’s seas, potentially driving coastal erosion,but the observational evidence of waves is indirect, and the processes affecting shoreline evolution on Titanremain unknown. No widely accepted framework exists for using shoreline morphology to quantitatively dis-cern coastal erosion mechanisms, even on Earth, where the dominant mechanisms are known. We combinelandscape evolution models with measurements of shoreline shape on Earth to characterize how differentcoastal erosion mechanisms affect shoreline morphology. Applying this framework to Titan, we find that theshorelines of Titan’s seas are most consistent with flooded landscapes that subsequently have been eroded bywaves, rather than a uniform erosional process or no coastal erosion, particularly if wave growth saturates atfetch lengths of tens of kilometers.
MICROBIAL INTERACTION PPT/ MICROBIAL INTERACTION AND THEIR TYPES // PLANT MIC...
MICROBIAL INTERACTION PPT/ MICROBIAL INTERACTION AND THEIR TYPES // PLANT MIC...ABHISHEK SONI NIMT INSTITUTE OF MEDICAL AND PARAMEDCIAL SCIENCES , GOVT PG COLLEGE NOIDA
Microbial interaction
Microorganisms interacts with each other and can be physically associated with another organisms in a variety of ways.
One organism can be located on the surface of another organism as an ectobiont or located within another organism as endobiont.
Microbial interaction may be positive such as mutualism, proto-cooperation, commensalism or may be negative such as parasitism, predation or competition
Types of microbial interaction
Positive interaction: mutualism, proto-cooperation, commensalism
Negative interaction: Ammensalism (antagonism), parasitism, predation, competition
I. Mutualism:
It is defined as the relationship in which each organism in interaction gets benefits from association. It is an obligatory relationship in which mutualist and host are metabolically dependent on each other.
Mutualistic relationship is very specific where one member of association cannot be replaced by another species.
Mutualism require close physical contact between interacting organisms.
Relationship of mutualism allows organisms to exist in habitat that could not occupied by either species alone.
Mutualistic relationship between organisms allows them to act as a single organism.
Examples of mutualism:
i. Lichens:
Lichens are excellent example of mutualism.
They are the association of specific fungi and certain genus of algae. In lichen, fungal partner is called mycobiont and algal partner is called
II. Syntrophism:
It is an association in which the growth of one organism either depends on or improved by the substrate provided by another organism.
In syntrophism both organism in association gets benefits.
Compound A
Utilized by population 1
Compound B
Utilized by population 2
Compound C
utilized by both Population 1+2
Products
In this theoretical example of syntrophism, population 1 is able to utilize and metabolize compound A, forming compound B but cannot metabolize beyond compound B without co-operation of population 2. Population 2is unable to utilize compound A but it can metabolize compound B forming compound C. Then both population 1 and 2 are able to carry out metabolic reaction which leads to formation of end product that neither population could produce alone.
Examples of syntrophism:
i. Methanogenic ecosystem in sludge digester
Methane produced by methanogenic bacteria depends upon interspecies hydrogen transfer by other fermentative bacteria.
Anaerobic fermentative bacteria generate CO2 and H2 utilizing carbohydrates which is then utilized by methanogenic bacteria (Methanobacter) to produce methane.
ii. Lactobacillus arobinosus and Enterococcus faecalis:
In the minimal media, Lactobacillus arobinosus and Enterococcus faecalis are able to grow together but not alone.
The synergistic relationship between E. faecalis and L. arobinosus occurs in which E. faecalis require folic acid
The cost of acquiring information by natural selection
This is a short talk that I gave at the Banff International Research Station workshop on Modeling and Theory in Population Biology. The idea is to try to understand how the burden of natural selection relates to the amount of information that selection puts into the genome.
It's based on the first part of this research paper:
The cost of information acquisition by natural selection
Ryan Seamus McGee, Olivia Kosterlitz, Artem Kaznatcheev, Benjamin Kerr, Carl T. Bergstrom
bioRxiv 2022.07.02.498577; doi: https://doi.org/10.1101/2022.07.02.498577
Evidence of Jet Activity from the Secondary Black Hole in the OJ 287 Binary S...
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Embracing Deep Variability For Reproducibility and Replicability
Embracing Deep Variability For Reproducibility and ReplicabilityUniversity of Rennes, INSA Rennes, Inria/IRISA, CNRS
Embracing Deep Variability For Reproducibility and Replicability
Abstract: Reproducibility (aka determinism in some cases) constitutes a fundamental aspect in various fields of computer science, such as floating-point computations in numerical analysis and simulation, concurrency models in parallelism, reproducible builds for third parties integration and packaging, and containerization for execution environments. These concepts, while pervasive across diverse concerns, often exhibit intricate inter-dependencies, making it challenging to achieve a comprehensive understanding. In this short and vision paper we delve into the application of software engineering techniques, specifically variability management, to systematically identify and explicit points of variability that may give rise to reproducibility issues (eg language, libraries, compiler, virtual machine, OS, environment variables, etc). The primary objectives are: i) gaining insights into the variability layers and their possible interactions, ii) capturing and documenting configurations for the sake of reproducibility, and iii) exploring diverse configurations to replicate, and hence validate and ensure the robustness of results. By adopting these methodologies, we aim to address the complexities associated with reproducibility and replicability in modern software systems and environments, facilitating a more comprehensive and nuanced perspective on these critical aspects.
https://hal.science/hal-04582287
一比一原版美国佩斯大学毕业证如何办理
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本公司拥有海外各大学样板无数，能完美还原。
1:1完美还原海外各大学毕业材料上的工艺：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。文字图案浮雕、激光镭射、紫外荧光、温感、复印防伪等防伪工艺。材料咨询办理、认证咨询办理请加学历顾问Q/微741003700
【主营项目】
一.毕业证【q微741003700】成绩单、使馆认证、教育部认证、雅思托福成绩单、学生卡等！
二.真实使馆公证(即留学回国人员证明,不成功不收费)
三.真实教育部学历学位认证（教育部存档！教育部留服网站永久可查）
四.办理各国各大学文凭(一对一专业服务,可全程监控跟踪进度)
如果您处于以下几种情况：
◇在校期间，因各种原因未能顺利毕业……拿不到官方毕业证【q/微741003700】
◇面对父母的压力，希望尽快拿到；
◇不清楚认证流程以及材料该如何准备；
◇回国时间很长，忘记办理；
◇回国马上就要找工作，办给用人单位看；
◇企事业单位必须要求办理的
◇需要报考公务员、购买免税车、落转户口
◇申请留学生创业基金
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
办理美国佩斯大学毕业证【微信：741003700 】外观非常简单，由纸质材料制成，上面印有校徽、校名、毕业生姓名、专业等信息。
办理美国佩斯大学毕业证【微信：741003700 】格式相对统一，各专业都有相应的模板。通常包括以下部分：
校徽：象征着学校的荣誉和传承。
校名:学校英文全称
授予学位：本部分将注明获得的具体学位名称。
毕业生姓名：这是最重要的信息之一，标志着该证书是由特定人员获得的。
颁发日期：这是毕业正式生效的时间，也代表着毕业生学业的结束。
其他信息：根据不同的专业和学位，可能会有一些特定的信息或章节。
办理美国佩斯大学毕业证【微信：741003700 】价值很高，需要妥善保管。一般来说，应放置在安全、干燥、防潮的地方，避免长时间暴露在阳光下。如需使用，最好使用复印件而不是原件，以免丢失。
综上所述，办理美国佩斯大学毕业证【微信：741003700 】是证明身份和学历的高价值文件。外观简单庄重，格式统一，包括重要的个人信息和发布日期。对持有人来说，妥善保管是非常重要的。
Anti-Universe And Emergent Gravity and the Dark Universe
Recent theoretical progress indicates that spacetime and gravity emerge together from the entanglement structure of an underlying microscopic theory. These ideas are best understood in Anti-de Sitter space, where they rely on the area law for entanglement entropy. The extension to de Sitter space requires taking into account the entropy and temperature associated with the cosmological horizon. Using insights from string theory, black hole physics and quantum information theory we argue that the positive dark energy leads to a thermal volume law contribution to the entropy that overtakes the area law precisely at the cosmological horizon. Due to the competition between area and volume law entanglement the microscopic de Sitter states do not thermalise at sub-Hubble scales: they exhibit memory effects in the form of an entropy displacement caused by matter. The emergent laws of gravity contain an additional ‘dark’ gravitational force describing the ‘elastic’ response due to the entropy displacement. We derive an estimate of the strength of this extra force in terms of the baryonic mass, Newton’s constant and the Hubble acceleration scale a0 = cH0, and provide evidence for the fact that this additional ‘dark gravity force’ explains the observed phenomena in galaxies and clusters currently attributed to dark matter.
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