The Richat Structure in Mauritania represents an eroded geologic dome comprised of sedimentary rocks from the late Proterozoic and Ordovician periods. While originally thought to be a meteorite impact structure, studies have found no evidence of shock processes. The structure likely formed from the uplift and erosion of an underlying alkaline magmatic body during the Cretaceous period. This research proposal aims to drill into the center of the structure to analyze rock compositions and better understand the subsurface geology and origin of the magmatic body through geophysical surveys and borehole data collection. Identifying the source and composition of the igneous rocks could help confirm or disprove the hypothesis of a subsurface intrusion related to continental ri
Influence of geological condition on foundation and design of buildingDarshan Darji
these ppt is about Influence of geological condition on foundation and design of building. This Ppt clear your doubt about this influence of geological condition on foundation and design of building.
Origin and Abundance of elements in the Solar system and in the Earth and its...AkshayRaut51
Definition of Elements and atom
Origin of Universe
Theories of origin of Solar system and Earth
Chemical Composition of Planets
Chemical Composition of Earth
Chemical composition of Meteorites
Abundance of Elements
Information about these fluids is an invaluable aid in mineral exploration.
Conventional academic methods of analysing fluid inclusions are too slow and tedious to be of practical application in typical mineral exploration activities.
However, the academic data from numerous studies does show that CO2 is an exceptionally important indicator when exploring for most types of gold deposit.
Because the baro-acoustic decrepitation method is a rapid and reliable method to measure CO2 contents in fluids, it can be used to study a spatial array of data and it is an invaluable and practical exploration method.
Measurements of temperatures of fluid inclusions does not usually help in mineral exploration as hydrothermal minerals deposit over a wide temperature range and there is no specific temperature which is indicative of mineralisation. However, if temperatures are available on a large spatial array of samples, then temperature trends may be a useful exploration method to find the hottest part of the system, which is presumably the location of the best economic mineralisation. Baro-acoustic decrepitation is the most practical method to determine temperatures of the large numbers of samples required.
Salinities of fluid inclusions are of limited use in exploration and are difficult to measure. However, they can be used to recognise intrusion related hydrothermal systems.
How can minerals deposits be formed; GEOLOGICAL PROCESSES; Ore Fluids; Ore Forming Processes; Concentrating Processes; Magmatic mineral deposits; Residual mineral deposits ; Placer deposits; Sedimentary mineral deposits; Metamorhogenic mineral deposits; Hydrothermal mineral deposits ; Magmatic Deposits
Cumulate deposits: fractional crystallization processes can concentrate metals (Cr, Fe, PGE, Pt, Ni, Ti, Diamond ))
Pegmatites : late staged crystallization forms pegmatites and many residual elements are concentrated (Li, Ce, Be, Sn, U, Rare Earths (REE), Feldspar, Mica, Gems).
magmatic deposits; Mode of Formation of Magmatic Ores Deposits; Mode of Formation of Orthomagmatic Ores ; Fractional Crystallization (or Crystal fractionation ); Magmatic (or Liquid ) Immiscibility; Simple crystallization without concentration (Dissemination); Segregation of early formed crystals; (Layer Types); Injection of material concentrated elsewhere by differentiation Residual liquid segregation; Residual liquid injection; Immiscible liquid segregation; Immiscible-liquid-injection; Early magmatic deposit; Late magmatic deposit; Types of Magmatic Ore Deposits:Chromite; Fe-Ti (± V) oxides; Ni – Cu – Fe (± Pt) sulfides; Platinum Group Elements (PGEs); REE, and Zr in Carbonatites; Diamond in kimberlites.
Influence of geological condition on foundation and design of buildingDarshan Darji
these ppt is about Influence of geological condition on foundation and design of building. This Ppt clear your doubt about this influence of geological condition on foundation and design of building.
Origin and Abundance of elements in the Solar system and in the Earth and its...AkshayRaut51
Definition of Elements and atom
Origin of Universe
Theories of origin of Solar system and Earth
Chemical Composition of Planets
Chemical Composition of Earth
Chemical composition of Meteorites
Abundance of Elements
Information about these fluids is an invaluable aid in mineral exploration.
Conventional academic methods of analysing fluid inclusions are too slow and tedious to be of practical application in typical mineral exploration activities.
However, the academic data from numerous studies does show that CO2 is an exceptionally important indicator when exploring for most types of gold deposit.
Because the baro-acoustic decrepitation method is a rapid and reliable method to measure CO2 contents in fluids, it can be used to study a spatial array of data and it is an invaluable and practical exploration method.
Measurements of temperatures of fluid inclusions does not usually help in mineral exploration as hydrothermal minerals deposit over a wide temperature range and there is no specific temperature which is indicative of mineralisation. However, if temperatures are available on a large spatial array of samples, then temperature trends may be a useful exploration method to find the hottest part of the system, which is presumably the location of the best economic mineralisation. Baro-acoustic decrepitation is the most practical method to determine temperatures of the large numbers of samples required.
Salinities of fluid inclusions are of limited use in exploration and are difficult to measure. However, they can be used to recognise intrusion related hydrothermal systems.
How can minerals deposits be formed; GEOLOGICAL PROCESSES; Ore Fluids; Ore Forming Processes; Concentrating Processes; Magmatic mineral deposits; Residual mineral deposits ; Placer deposits; Sedimentary mineral deposits; Metamorhogenic mineral deposits; Hydrothermal mineral deposits ; Magmatic Deposits
Cumulate deposits: fractional crystallization processes can concentrate metals (Cr, Fe, PGE, Pt, Ni, Ti, Diamond ))
Pegmatites : late staged crystallization forms pegmatites and many residual elements are concentrated (Li, Ce, Be, Sn, U, Rare Earths (REE), Feldspar, Mica, Gems).
magmatic deposits; Mode of Formation of Magmatic Ores Deposits; Mode of Formation of Orthomagmatic Ores ; Fractional Crystallization (or Crystal fractionation ); Magmatic (or Liquid ) Immiscibility; Simple crystallization without concentration (Dissemination); Segregation of early formed crystals; (Layer Types); Injection of material concentrated elsewhere by differentiation Residual liquid segregation; Residual liquid injection; Immiscible liquid segregation; Immiscible-liquid-injection; Early magmatic deposit; Late magmatic deposit; Types of Magmatic Ore Deposits:Chromite; Fe-Ti (± V) oxides; Ni – Cu – Fe (± Pt) sulfides; Platinum Group Elements (PGEs); REE, and Zr in Carbonatites; Diamond in kimberlites.
Applied Mineralogy
Technical Mineralogy;
How much metal is available?
What is a mineral?
What is Applied Mineralogy?
What Applied Mineralogy is not…
History
Review of some mineralogical Concepts
Plate tectonics, like crustal evolution, provides a basis for understanding the distribution and origin of mineral and energy deposits. Different types of ores are characterized by distinct geological environment and tectonic settings.
Manganese ore deposits are widely scattered in various districts in Egypt.
They occur at some localities in Sinai Peninsula and at a few localities in the Eastern Desert.
Manganese deposits are known:
in the Um Bogma district in west central Sinai; and
in the Halaib "Elba" district in the southern portion of Eastern Desert.
In addition, minor occurrences are known in Wadi Mialik near Abu Ghosun and Ras Banas in the Southern Eastern Desert, and Wadi Abu Shaar El Qibli (Black Hill), to the north of Hurghada
To review the geology of rare earth elements.
To discuss the various applications of rare earth elements in geological studies.
To review the geology of rare earth elements.
To discuss the various applications of rare earth elements in geological studies.
Abundance of REEs in Earth’s Crust ; Classification of Rare Earth Elements; Geology of REEs; APPLICATIONS OF REES; Application OF REEs in Geological Studies; APPLICATION OF REE TO PETROLEUM SYSTEMS; REE GLOBAL ECONOMIC SUPPLY AND DEMAND; Large and Giant Sized Deposits of the Rare Earth Elements
Application of Basic Remote Sensing in GeologyUzair Khan
Application of basic remote sensing in Geology. This presentation tries to discriminate the lithology in the Landsat-7 scene located Karachi West. Although other enhanced methodology available to discriminate the rock types, here just a band ratios and simple band combination used for lithology identification.
Minerals are formed by changes in chemical energy in systems which contain one fluid or vapor phase. In nature, minerals are formed by crystallisation or precipitation from concentrated solutions. These solutions are called as ore-bearing fluids. Ore-bearing fluids are characterised by high concentration of certain metallic or other elements.
Fluids are the most effective agents for the transport of material in the mantle and the Earth's crust.
rubidium strontium dating method . introduction. decay scheme. formation of isochrons. tracking of initial sr isotopes ratios. drawbacks and uses of Rb Sr method.
Journal Petroleum Geology. Northern and Central North Sea Aptian sands, lowstand systems tract. Sequence stratigraphy development, Logs and micropapaeontology. prospectivity
Hawaii's Most Active Volcano: Here's The Latest On Kilauea's Eruption
The Kilauea volcano is located in the southeastern part of the Big Island of Hawaii.
Believe it or not, Kilauea has been erupting continuously since 1983, with only occasional pauses of quiet activity. This particular "episode" of the eruption began in the late afternoon of May 3, in a part of Leilani Estates, a subdivision near the town of Pahoa.
Officials said there is no way to predict how long the eruption will continue or what shape it will take. This eruption could be finished or could go on for a long time.
Kilauea is one of the most active and well-monitored volcanoes in the world. It's been erupting on and off for hundreds of thousands of years.
All of Hawaii is a tourist destination, but this particular eruption wasn't in an area where most tourists go. The homes at risk are in a subdivision near the town of Pahoa.
Source: USA TODAY. By Doyle Rice. May 4, 2018, accessed May 5, 2018
<https://www.usatoday.com/story/news/nation/2018/05/04/hawaii-volcano-eruption-kilauea-big-island/580466002/>
________________________
Kilauea Volcano Erupts, Spewing Lava and Gases Near Homes in Hawaii
Governor David Ige has issued an emergency proclamation and has called up the National Guard to help emergency workers with evacuation efforts.
Source: THE NEW YORK TIMES. By Meghan Miner Murray, Sabrina Tavernise and Maya Salam. May 4, 2018, accessed May 5, 2018
<https://www.nytimes.com/2018/05/04/us/kilauea-volcano-eruption-hawaii.html>
Applied Mineralogy
Technical Mineralogy;
How much metal is available?
What is a mineral?
What is Applied Mineralogy?
What Applied Mineralogy is not…
History
Review of some mineralogical Concepts
Plate tectonics, like crustal evolution, provides a basis for understanding the distribution and origin of mineral and energy deposits. Different types of ores are characterized by distinct geological environment and tectonic settings.
Manganese ore deposits are widely scattered in various districts in Egypt.
They occur at some localities in Sinai Peninsula and at a few localities in the Eastern Desert.
Manganese deposits are known:
in the Um Bogma district in west central Sinai; and
in the Halaib "Elba" district in the southern portion of Eastern Desert.
In addition, minor occurrences are known in Wadi Mialik near Abu Ghosun and Ras Banas in the Southern Eastern Desert, and Wadi Abu Shaar El Qibli (Black Hill), to the north of Hurghada
To review the geology of rare earth elements.
To discuss the various applications of rare earth elements in geological studies.
To review the geology of rare earth elements.
To discuss the various applications of rare earth elements in geological studies.
Abundance of REEs in Earth’s Crust ; Classification of Rare Earth Elements; Geology of REEs; APPLICATIONS OF REES; Application OF REEs in Geological Studies; APPLICATION OF REE TO PETROLEUM SYSTEMS; REE GLOBAL ECONOMIC SUPPLY AND DEMAND; Large and Giant Sized Deposits of the Rare Earth Elements
Application of Basic Remote Sensing in GeologyUzair Khan
Application of basic remote sensing in Geology. This presentation tries to discriminate the lithology in the Landsat-7 scene located Karachi West. Although other enhanced methodology available to discriminate the rock types, here just a band ratios and simple band combination used for lithology identification.
Minerals are formed by changes in chemical energy in systems which contain one fluid or vapor phase. In nature, minerals are formed by crystallisation or precipitation from concentrated solutions. These solutions are called as ore-bearing fluids. Ore-bearing fluids are characterised by high concentration of certain metallic or other elements.
Fluids are the most effective agents for the transport of material in the mantle and the Earth's crust.
rubidium strontium dating method . introduction. decay scheme. formation of isochrons. tracking of initial sr isotopes ratios. drawbacks and uses of Rb Sr method.
Journal Petroleum Geology. Northern and Central North Sea Aptian sands, lowstand systems tract. Sequence stratigraphy development, Logs and micropapaeontology. prospectivity
Hawaii's Most Active Volcano: Here's The Latest On Kilauea's Eruption
The Kilauea volcano is located in the southeastern part of the Big Island of Hawaii.
Believe it or not, Kilauea has been erupting continuously since 1983, with only occasional pauses of quiet activity. This particular "episode" of the eruption began in the late afternoon of May 3, in a part of Leilani Estates, a subdivision near the town of Pahoa.
Officials said there is no way to predict how long the eruption will continue or what shape it will take. This eruption could be finished or could go on for a long time.
Kilauea is one of the most active and well-monitored volcanoes in the world. It's been erupting on and off for hundreds of thousands of years.
All of Hawaii is a tourist destination, but this particular eruption wasn't in an area where most tourists go. The homes at risk are in a subdivision near the town of Pahoa.
Source: USA TODAY. By Doyle Rice. May 4, 2018, accessed May 5, 2018
<https://www.usatoday.com/story/news/nation/2018/05/04/hawaii-volcano-eruption-kilauea-big-island/580466002/>
________________________
Kilauea Volcano Erupts, Spewing Lava and Gases Near Homes in Hawaii
Governor David Ige has issued an emergency proclamation and has called up the National Guard to help emergency workers with evacuation efforts.
Source: THE NEW YORK TIMES. By Meghan Miner Murray, Sabrina Tavernise and Maya Salam. May 4, 2018, accessed May 5, 2018
<https://www.nytimes.com/2018/05/04/us/kilauea-volcano-eruption-hawaii.html>
Seismic Reflection Surveys in Search for Iron Oxide Copper-Gold (IOCG) Depositsiosrjce
Seismic reflection method can delineate very complex geological structures hence it might be very
effective for detecting the presence of Iron Oxide Copper-Gold (IOCG) deposits. Despite this superior
attributes, there exist a real problem for exploration beyond the immediate vicinity of a known deposit. All
previous studies have focused upon high resolution detection of mineralization and the hosting structures at
mine scale. No argument for “regional” exploration have been proposed probably because a cost benefit
analysis has never be conducted at such scale to proceed with such exploration venture. In this study, we
analyze the feasibility of such regional exploration by modelling a Vulcan IOCGU deposit scenario were a 2D
seismic survey with relatively sparse source-receiver geometry was used to detect the presence of a possible
intrusive package within 2km depth range. The modelling results demonstrates that seismic reflection method
using 10m geophones and 20m shot spacing can be used to image deposit within the depth of 2km. The
presence of reflections was visibly observed especially at the edges of intrusive packages hence it is suggested
that application of seismic reflection methods perhaps will remains the best alternative and most viable method
for exploring deep seated IOCG
Connector Corner: Automate dynamic content and events by pushing a buttonDianaGray10
Here is something new! In our next Connector Corner webinar, we will demonstrate how you can use a single workflow to:
Create a campaign using Mailchimp with merge tags/fields
Send an interactive Slack channel message (using buttons)
Have the message received by managers and peers along with a test email for review
But there’s more:
In a second workflow supporting the same use case, you’ll see:
Your campaign sent to target colleagues for approval
If the “Approve” button is clicked, a Jira/Zendesk ticket is created for the marketing design team
But—if the “Reject” button is pushed, colleagues will be alerted via Slack message
Join us to learn more about this new, human-in-the-loop capability, brought to you by Integration Service connectors.
And...
Speakers:
Akshay Agnihotri, Product Manager
Charlie Greenberg, Host
Transcript: Selling digital books in 2024: Insights from industry leaders - T...BookNet Canada
The publishing industry has been selling digital audiobooks and ebooks for over a decade and has found its groove. What’s changed? What has stayed the same? Where do we go from here? Join a group of leading sales peers from across the industry for a conversation about the lessons learned since the popularization of digital books, best practices, digital book supply chain management, and more.
Link to video recording: https://bnctechforum.ca/sessions/selling-digital-books-in-2024-insights-from-industry-leaders/
Presented by BookNet Canada on May 28, 2024, with support from the Department of Canadian Heritage.
UiPath Test Automation using UiPath Test Suite series, part 4DianaGray10
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The UiPath Test Manager overview with SAP heatmap webinar offers a concise yet comprehensive exploration of the role of a Test Manager within SAP environments, coupled with the utilization of heatmaps for effective testing strategies.
Participants will gain insights into the responsibilities, challenges, and best practices associated with test management in SAP projects. Additionally, the webinar delves into the significance of heatmaps as a visual aid for identifying testing priorities, areas of risk, and resource allocation within SAP landscapes. Through this session, attendees can expect to enhance their understanding of test management principles while learning practical approaches to optimize testing processes in SAP environments using heatmap visualization techniques
What will you get from this session?
1. Insights into SAP testing best practices
2. Heatmap utilization for testing
3. Optimization of testing processes
4. Demo
Topics covered:
Execution from the test manager
Orchestrator execution result
Defect reporting
SAP heatmap example with demo
Speaker:
Deepak Rai, Automation Practice Lead, Boundaryless Group and UiPath MVP
Slack (or Teams) Automation for Bonterra Impact Management (fka Social Soluti...Jeffrey Haguewood
Sidekick Solutions uses Bonterra Impact Management (fka Social Solutions Apricot) and automation solutions to integrate data for business workflows.
We believe integration and automation are essential to user experience and the promise of efficient work through technology. Automation is the critical ingredient to realizing that full vision. We develop integration products and services for Bonterra Case Management software to support the deployment of automations for a variety of use cases.
This video focuses on the notifications, alerts, and approval requests using Slack for Bonterra Impact Management. The solutions covered in this webinar can also be deployed for Microsoft Teams.
Interested in deploying notification automations for Bonterra Impact Management? Contact us at sales@sidekicksolutionsllc.com to discuss next steps.
Search and Society: Reimagining Information Access for Radical FuturesBhaskar Mitra
The field of Information retrieval (IR) is currently undergoing a transformative shift, at least partly due to the emerging applications of generative AI to information access. In this talk, we will deliberate on the sociotechnical implications of generative AI for information access. We will argue that there is both a critical necessity and an exciting opportunity for the IR community to re-center our research agendas on societal needs while dismantling the artificial separation between the work on fairness, accountability, transparency, and ethics in IR and the rest of IR research. Instead of adopting a reactionary strategy of trying to mitigate potential social harms from emerging technologies, the community should aim to proactively set the research agenda for the kinds of systems we should build inspired by diverse explicitly stated sociotechnical imaginaries. The sociotechnical imaginaries that underpin the design and development of information access technologies needs to be explicitly articulated, and we need to develop theories of change in context of these diverse perspectives. Our guiding future imaginaries must be informed by other academic fields, such as democratic theory and critical theory, and should be co-developed with social science scholars, legal scholars, civil rights and social justice activists, and artists, among others.
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I have heard many times that architecture is not important for the front-end. Also, many times I have seen how developers implement features on the front-end just following the standard rules for a framework and think that this is enough to successfully launch the project, and then the project fails. How to prevent this and what approach to choose? I have launched dozens of complex projects and during the talk we will analyze which approaches have worked for me and which have not.
The Art of the Pitch: WordPress Relationships and SalesLaura Byrne
Clients don’t know what they don’t know. What web solutions are right for them? How does WordPress come into the picture? How do you make sure you understand scope and timeline? What do you do if sometime changes?
All these questions and more will be explored as we talk about matching clients’ needs with what your agency offers without pulling teeth or pulling your hair out. Practical tips, and strategies for successful relationship building that leads to closing the deal.
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Keynote at DIGIT West Expo, Glasgow on 29 May 2024.
Cheryl Hung, ochery.com
Sr Director, Infrastructure Ecosystem, Arm.
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All of this illustrated with link prediction over knowledge graphs, but the argument is general.
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DevOps and Testing slides at DASA ConnectKari Kakkonen
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FIDO Alliance Osaka Seminar: The WebAuthn API and Discoverable Credentials.pdf
The richat structure
1. Callum Thurley The Richat Structure Research Proposal
Page 1 of 3
The Formation of the Richat Structure
Introduction
The Richat Structure or the “Eye of the
Sahara” is somewhat of an enigma to
geologists today. It is 40km in diameter,
and represents 3 major rings dipping
outward from the centre of the structure.
This circular feature representsan eroded
geologic dome, with sedimentary rocks of
late Proterozoic and Ordovician Age.
The Problem
The origin of theRichat Structure and the underlying magmatic body is not fully
understood, and this project main objective is to solve this. Originally it was thought
to be a meteorite impact structure, however studies undertaken by Robert S Dietz et
al 1968confirm that there aren’t any features that would commonly be associated
with “shock processes”, and therefore this cannot be an impact structure.
General Lithologies
The centre of the Richat Structure is comprised of a limestone-dolomite shelf that
encircles a large scale Breccia that was formed by Karstdissolution and collapse. Due
to the presence of neo-formed Cretaceous K-Feldspar it has been interpreted that
these sediments have a hydrothermal origin of Cretaceous age. Basaltic ring dykes,
Kimberlites, and alkaline volcanic rocks intrude and post-date these internal
sediments further suggesting that there was an alkaline magmatic body beneath the
Richat Structure (Matton et al 2005).
Current Hypothesis
The origin of the RichatStrucure
has been hypothesised as an
eroded anticlinal dome, however
its formation is not entirely
understood. It is also thought
that there is an underlying large
alkaline magmatic body, and this
project will hopefully prove or
disprove this.
The injection of an alkaline
magma occurred during the
Cretaceous period (Matton et al
2005), at this time the position of
the North Western African
continent was near to the Southern Atlantic Ocean during the oceans embryonic
stages of spreading (Figure 2). This is a rather peculiar location to find an alkaline
Figure 1 – An aerial photograph of the Richat
Structure.
Figure 1 – An image of the Richat Structure.
Previously the mineral Barite was misinterpreted for Coesite, a mineral that is
indicative of shock metamorphism from high velocity extraterrestrial impacts.
It probably represented a shear zone that developed in tectonic doming rather
than a meteorite impact (R.F.Fudali 1969).
Figure 2 – A continental reconstruction from the late
Cretaceous (Doucoure and de Wit 2003)
2. Callum Thurley The Richat Structure Research Proposal
Page 2 of 3
magma, because alkali magmas are usually associated with continental rift systems
such as in East Africa, however there isn’t a rift system in close proximity to the
Richat Structure. The Injection of this alkaline magma may have occurred due to the
extension and thinning of the crust near Mauritania.. It has been hypothesised that
the magmatism may be attributed to a mantle plume, heating the base of this thinned
crust (Collins 2011)These two factors combined together are the most likely cause of
continental alkali magmatism. The opening of the Atlantic has been attributed to
plume activity and lead to the formation of the Peri-Atlantic Alkaline Province where
the Richat Structure is located (Matton 2008). The presence of Kimberlites is not
surprising, due to the fact that some of the oldest crust in the world is located in the
western African Craton, a typical tectonic setting for Kimberlites. Finally it may have
been the upwelling of this magma that caused up warping and doming of the
overlying sediments. This can be inferred because there is not any kind of
convergent plate boundary in close proximity to produce fold tectonically.
This Project and Methodology
The proposed drilling site for thisproject is at the centre of the structure (as seen
above in Figure 3) at the approximate GPS co-ordinates of 21°07’30” N, 11°24’00”
W.This project plans to drill a borehole approximately 20km into the structure to
penetrate into the magmatic body below(Matton 2008). Enabling us to identify
exactly what the source of the ring dykes are by geochemical analysis, such as the
LREE, HREE, LILE, and incompatible elemental compositions of the magmatic body.
This may also
unearth data that has
not previously been
seen, such as the
subsurface
lithologies. It will
either confirm or
disprove the
presence of a
subsurface intrusion
and identify its
source. Furthermore,
we can compare the
composition of the
alkali magma with
that of other magmas
Figure 3 – A photograph showing the proposed drilling site. (Google Earth Copyright
2013)
Figure 4 – Cross Section of the Richat Structure (Matton)
2008)
3. Callum Thurley The Richat Structure Research Proposal
Page 3 of 3
that have identified sources. This data can then be correlated with the rocks brought
up from within the borehole.Elemental similarities between these samples and other
igneous rocks with known sources can be identified and interpreted.
Geophysical Data
Shallow and deep seismic profiling will have to be carried out here. Both of these
datasets will becorrelated with borehole lithological data to work out an accurate
cross section. This will enable us to have a deeper understanding of the subsurface
geology, and ultimately it will allow us to understand the processes of its formation.
If possible three dimensional profiling of the crust here would be perfect because it
would give us a further insight into the details of structures below the Richat
Structure. A Magnetic survey could be carried out, which would be useful because
the minerals within the igneous rocks would have a higher magnetic signal than that
of the country rock. Therefore this would give us some indication of where to drill. A
gravity survey will also be carried out, due to the fact that the intruded igneous rocks
would have a higher specific gravity than the country rock, therefore giving more
detail about the location of the magmatic body.
Problems
A Possible problem with the project is that the magmatic body may not be
directly below the centre of structure itself, and so drilling may not enable us
to locate the source of the igneous lithologies.Doing the initialgeophysical
survey and then drilling would solve this.
Conditions in the Sahara may provide some issues, mainly the temperature
would be an issue, where in the summer the temperature regularly exceeds
50°C. This could lead to dehydration of the research scientists, however very
simply always carry sufficient water, or just carrying out the research in the
winter months could solve this.
References
1. Collins, S 2012, Balance sheets, lecture notes distributed in Igneous and
Metamorphic Geochemistry and Petrology, at The University of Durham,
2012.
2. Richat and Semsiyat Domes (Mauritania): Not Astroblemes, Robert S Dietz,
Robert Fudali, and William Casidy, December 1968. doi: 10.1130/ 0016-7606, v.
80 no. 7 p. 1367-1372
3. Old inherited origin for the present near-bimodal topography of Africa,
C.MoctarDoucouré, Maarten J. de Wit, Volume 36, Issue 4, May 2003, Pages
371–388.
4. Coesite from the Richat Dome, Mauritania: A Misinterpretation, R.F.Fudali,
10th
October1969, vol-166, no.3902, pp 228-30
5. Google Earth Copyright 2013.
6. Jones and Bartlett. Boston. Winter (2001) An Introduction to Igneous and
Metamorphic Petrology. Prentice Hall.
7. Resolving the Richat enigma: Doming and hydrothermal karstification above an
alkaline complex , Guillaume Matton, Michel Jebrak and James K.W.Lee,
2005.doi: 10.1130/G21542AR.1, v. 33 no. 8 p. 665-668
8. The Cretaceous Complex of Richat (Mauritania); A Peri-Atlantic Alkaline
Process,,GuillaumeMatton 2008,
If the rocks have a chemical signature that is enriched in incompatible elements,
then we can confirm that it has a deeper mantle source, similar to that of OIB.