High potential geothermal areas within the Rahat volcanic field, Saudi Arabia, from gravity data and 3D geological modeling
We present various geological models to examine the geothermal energy potential at the Rahat volcanic field, Saudi Arabia. The method involves the application of geophysical techniques of gravity and seismic tomography results to derive a 3D subsurface geological structure representing possible subs...
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creator | Aboud, Essam Abraham, Ema Alqahtani, Faisal Abdulfarraj, Murad |
description | We present various geological models to examine the geothermal energy potential at the Rahat volcanic field, Saudi Arabia. The method involves the application of geophysical techniques of gravity and seismic tomography results to derive a 3D subsurface geological structure representing possible subsurface structural information beneath the northern Rahat volcanic field. Results show a secluded subsurface structure within the basement crust with low densities (
2800
kg
/
m
3
)
and low
P
-wave velocity structure. Identified secluded subsurface structure could depict a magma intrusion within the basement and its depth proximity to the basalt deposition in the region signals the viability of this location for geothermal exploration. Deductions also show that the geothermal reservoir could be reached at starting depths of ~ 1.3 km, whereas its effect could be accessed at depths
<
1
km. Within the geothermal active region of northern Harrat Rahat, this study has suggested possible locations with high potential for further geothermal exploration. |
doi_str_mv | 10.1007/s11600-023-01182-6 |
format | Article |
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kg
/
m
3
) and a slightly high
P
-wave velocity, enclosed by a high density
(
>
2800
kg
/
m
3
)
and low
P
-wave velocity structure. Identified secluded subsurface structure could depict a magma intrusion within the basement and its depth proximity to the basalt deposition in the region signals the viability of this location for geothermal exploration. Deductions also show that the geothermal reservoir could be reached at starting depths of ~ 1.3 km, whereas its effect could be accessed at depths
<
1
km. Within the geothermal active region of northern Harrat Rahat, this study has suggested possible locations with high potential for further geothermal exploration.</description><identifier>ISSN: 1895-7455</identifier><identifier>ISSN: 1895-6572</identifier><identifier>EISSN: 1895-7455</identifier><identifier>DOI: 10.1007/s11600-023-01182-6</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Basalt ; Basements ; Earth and Environmental Science ; Earth Sciences ; Geological structures ; Geology ; Geophysical methods ; Geophysics/Geodesy ; Geotechnical Engineering & Applied Earth Sciences ; Geothermal energy ; Geothermal resources ; Magma ; P waves ; Research Article - Applied Geophysics ; Seismic wave velocities ; Structural Geology ; Three dimensional models ; Volcanic fields ; Wave velocity</subject><ispartof>Acta geophysica, 2024-06, Vol.72 (3), p.1713-1729</ispartof><rights>The Author(s) under exclusive licence to Institute of Geophysics, Polish Academy of Sciences & Polish Academy of Sciences 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c270t-1aedc2be7dc5166e977bbd17a9fc908f1e47184eb98ba2a8ce5775ce88ac90b93</cites><orcidid>0000-0003-0623-5604</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11600-023-01182-6$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11600-023-01182-6$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Aboud, Essam</creatorcontrib><creatorcontrib>Abraham, Ema</creatorcontrib><creatorcontrib>Alqahtani, Faisal</creatorcontrib><creatorcontrib>Abdulfarraj, Murad</creatorcontrib><title>High potential geothermal areas within the Rahat volcanic field, Saudi Arabia, from gravity data and 3D geological modeling</title><title>Acta geophysica</title><addtitle>Acta Geophys</addtitle><description>We present various geological models to examine the geothermal energy potential at the Rahat volcanic field, Saudi Arabia. The method involves the application of geophysical techniques of gravity and seismic tomography results to derive a 3D subsurface geological structure representing possible subsurface structural information beneath the northern Rahat volcanic field. Results show a secluded subsurface structure within the basement crust with low densities (< 2500
kg
/
m
3
) and a slightly high
P
-wave velocity, enclosed by a high density
(
>
2800
kg
/
m
3
)
and low
P
-wave velocity structure. Identified secluded subsurface structure could depict a magma intrusion within the basement and its depth proximity to the basalt deposition in the region signals the viability of this location for geothermal exploration. Deductions also show that the geothermal reservoir could be reached at starting depths of ~ 1.3 km, whereas its effect could be accessed at depths
<
1
km. Within the geothermal active region of northern Harrat Rahat, this study has suggested possible locations with high potential for further geothermal exploration.</description><subject>Basalt</subject><subject>Basements</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geological structures</subject><subject>Geology</subject><subject>Geophysical methods</subject><subject>Geophysics/Geodesy</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Geothermal energy</subject><subject>Geothermal resources</subject><subject>Magma</subject><subject>P waves</subject><subject>Research Article - Applied Geophysics</subject><subject>Seismic wave velocities</subject><subject>Structural Geology</subject><subject>Three dimensional models</subject><subject>Volcanic fields</subject><subject>Wave velocity</subject><issn>1895-7455</issn><issn>1895-6572</issn><issn>1895-7455</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp9kEtPwzAQhCMEEqXwBzhZ4tqAnZedY1UeRaqExONsbZxN4iqJi-0WVfx5UoIEJ0472p35VpoguGT0mlHKbxxjGaUhjeKQMiaiMDsKJkzkaciTND3-o0-DM-fWlGYJZdEk-FzquiEb47H3GlpSo_EN2m6QYBEc-dC-0T0ZluQZGvBkZ1oFvVak0tiWM_IC21KTuYVCw4xU1nSktrDTfk9K8ECgL0l8ewC3ptZqAHemxFb39XlwUkHr8OJnToO3-7vXxTJcPT08LuarUEWc-pABlioqkJcqZVmGOedFUTIOeaVyKiqGCWciwSIXBUQgFKacpwqFgOFe5PE0uBq5G2vet-i8XJut7YeXMqaJ4Gmas4MrGl3KGucsVnJjdQd2LxmVh5LlWLIcSpbfJctsCMVjyA3mvkb7i_4n9QWb14DA</recordid><startdate>20240601</startdate><enddate>20240601</enddate><creator>Aboud, Essam</creator><creator>Abraham, Ema</creator><creator>Alqahtani, Faisal</creator><creator>Abdulfarraj, Murad</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KL.</scope><scope>KR7</scope><scope>L7M</scope><orcidid>https://orcid.org/0000-0003-0623-5604</orcidid></search><sort><creationdate>20240601</creationdate><title>High potential geothermal areas within the Rahat volcanic field, Saudi Arabia, from gravity data and 3D geological modeling</title><author>Aboud, Essam ; Abraham, Ema ; Alqahtani, Faisal ; Abdulfarraj, Murad</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c270t-1aedc2be7dc5166e977bbd17a9fc908f1e47184eb98ba2a8ce5775ce88ac90b93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Basalt</topic><topic>Basements</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geological structures</topic><topic>Geology</topic><topic>Geophysical methods</topic><topic>Geophysics/Geodesy</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Geothermal energy</topic><topic>Geothermal resources</topic><topic>Magma</topic><topic>P waves</topic><topic>Research Article - Applied Geophysics</topic><topic>Seismic wave velocities</topic><topic>Structural Geology</topic><topic>Three dimensional models</topic><topic>Volcanic fields</topic><topic>Wave velocity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Aboud, Essam</creatorcontrib><creatorcontrib>Abraham, Ema</creatorcontrib><creatorcontrib>Alqahtani, Faisal</creatorcontrib><creatorcontrib>Abdulfarraj, Murad</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Acta geophysica</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Aboud, Essam</au><au>Abraham, Ema</au><au>Alqahtani, Faisal</au><au>Abdulfarraj, Murad</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>High potential geothermal areas within the Rahat volcanic field, Saudi Arabia, from gravity data and 3D geological modeling</atitle><jtitle>Acta geophysica</jtitle><stitle>Acta Geophys</stitle><date>2024-06-01</date><risdate>2024</risdate><volume>72</volume><issue>3</issue><spage>1713</spage><epage>1729</epage><pages>1713-1729</pages><issn>1895-7455</issn><issn>1895-6572</issn><eissn>1895-7455</eissn><abstract>We present various geological models to examine the geothermal energy potential at the Rahat volcanic field, Saudi Arabia. The method involves the application of geophysical techniques of gravity and seismic tomography results to derive a 3D subsurface geological structure representing possible subsurface structural information beneath the northern Rahat volcanic field. Results show a secluded subsurface structure within the basement crust with low densities (< 2500
kg
/
m
3
) and a slightly high
P
-wave velocity, enclosed by a high density
(
>
2800
kg
/
m
3
)
and low
P
-wave velocity structure. Identified secluded subsurface structure could depict a magma intrusion within the basement and its depth proximity to the basalt deposition in the region signals the viability of this location for geothermal exploration. Deductions also show that the geothermal reservoir could be reached at starting depths of ~ 1.3 km, whereas its effect could be accessed at depths
<
1
km. Within the geothermal active region of northern Harrat Rahat, this study has suggested possible locations with high potential for further geothermal exploration.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s11600-023-01182-6</doi><tpages>17</tpages><orcidid>https://orcid.org/0000-0003-0623-5604</orcidid></addata></record> |
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source | SpringerLink Journals - AutoHoldings |
subjects | Basalt Basements Earth and Environmental Science Earth Sciences Geological structures Geology Geophysical methods Geophysics/Geodesy Geotechnical Engineering & Applied Earth Sciences Geothermal energy Geothermal resources Magma P waves Research Article - Applied Geophysics Seismic wave velocities Structural Geology Three dimensional models Volcanic fields Wave velocity |
title | High potential geothermal areas within the Rahat volcanic field, Saudi Arabia, from gravity data and 3D geological modeling |
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