Loading…
Crustal structure of the Volgo–Uralian subcraton revealed by inverse and forward gravity modelling
Volgo-Uralia is a Neoarchaean easternmost part of the East European craton. Recent seismic studies of the Volgo-Uralian region provided new insights into the crustal structure of this area. In this study, we combine satellite gravity and seismic data in a common workflow to perform a complex study o...
Saved in:
Published in: | Solid earth (Göttingen) 2022-03, Vol.13 (2), p.431-448 |
---|---|
Main Authors: | , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | cdi_FETCH-LOGICAL-c474t-6a8f2451eb37a1dc8aa97ebcbc02bdae42cf66acf7cab662b34d9d4c204946e23 |
---|---|
cites | cdi_FETCH-LOGICAL-c474t-6a8f2451eb37a1dc8aa97ebcbc02bdae42cf66acf7cab662b34d9d4c204946e23 |
container_end_page | 448 |
container_issue | 2 |
container_start_page | 431 |
container_title | Solid earth (Göttingen) |
container_volume | 13 |
creator | Ognev, Igor Ebbing, Jörg Haas, Peter |
description | Volgo-Uralia is a Neoarchaean easternmost part of the East European craton. Recent seismic studies of the Volgo-Uralian region provided new insights into the crustal structure of this area. In this study, we combine satellite gravity and seismic data in a common workflow to perform a complex study of Volgo-Uralian crustal structure, which is useful for further basin analysis of the area. In this light, a new crustal model of the Volgo-Uralian subcraton is presented from a step-wise approach: (1) inverse gravity modelling followed by (2) 3D forward gravity modelling. |
doi_str_mv | 10.5194/se-13-431-2022 |
format | article |
fullrecord | <record><control><sourceid>gale_doaj_</sourceid><recordid>TN_cdi_doaj_primary_oai_doaj_org_article_2c4d5dfc049a43d2b5e74a54a5442a12</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A695479447</galeid><doaj_id>oai_doaj_org_article_2c4d5dfc049a43d2b5e74a54a5442a12</doaj_id><sourcerecordid>A695479447</sourcerecordid><originalsourceid>FETCH-LOGICAL-c474t-6a8f2451eb37a1dc8aa97ebcbc02bdae42cf66acf7cab662b34d9d4c204946e23</originalsourceid><addsrcrecordid>eNptUk1v1DAQjRBIVKVXzpY4cUiJP-JsjtWKj5UqIQHlak3scfAqG5exs3Rv_Af-YX9JvRQBlToeaazRe2_G1quql7w5b3mv3iSsuayV5LVohHhSnfCV7uu-Ff3T_-7Pq7OUtk0J3YmulSeVW9OSMkwsZVpsXghZ9Cx_Q_Y1TmO8_fnrimAKMLO0DJYgx5kR7hEmdGw4sDDvkRIymB3zkX4AOTYS7EM-sF10OE1hHl9UzzxMCc_-1NPq6t3bL-sP9eXH95v1xWVtVadyrWHlhWo5DrID7uwKoO9wsINtxOAAlbBea7C-szBoLQapXO-UFY3qlUYhT6vNva6LsDXXFHZABxMhmN-NSKMBysFOaIRVrnXeFioo6cTQYqegPaYSwI9ar-61ril-XzBls40LzWV9I7RUukwUq3-osXyICbOPmcDuQrLmQvet6nqluoI6fwRVjsNdsHFGH0r_AeH1A0LBZLzJIywpmc3nT4-KW4opEfq_D-eNOXrDJDRcmuINc_SGvAM9iqzB</addsrcrecordid><sourcetype>Open Website</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2634694628</pqid></control><display><type>article</type><title>Crustal structure of the Volgo–Uralian subcraton revealed by inverse and forward gravity modelling</title><source>Publicly Available Content Database</source><creator>Ognev, Igor ; Ebbing, Jörg ; Haas, Peter</creator><creatorcontrib>Ognev, Igor ; Ebbing, Jörg ; Haas, Peter</creatorcontrib><description>Volgo-Uralia is a Neoarchaean easternmost part of the East European craton. Recent seismic studies of the Volgo-Uralian region provided new insights into the crustal structure of this area. In this study, we combine satellite gravity and seismic data in a common workflow to perform a complex study of Volgo-Uralian crustal structure, which is useful for further basin analysis of the area. In this light, a new crustal model of the Volgo-Uralian subcraton is presented from a step-wise approach: (1) inverse gravity modelling followed by (2) 3D forward gravity modelling.</description><identifier>ISSN: 1869-9529</identifier><identifier>ISSN: 1869-9510</identifier><identifier>EISSN: 1869-9529</identifier><identifier>DOI: 10.5194/se-13-431-2022</identifier><language>eng</language><publisher>Gottingen: Copernicus GmbH</publisher><subject>Analysis ; Constraint modelling ; Cratons ; Crust ; Crustal structure ; Crustal thickness ; Density ; Earth ; Earth science ; Gravitational fields ; Gravity anomalies ; Gravity field ; Mantle ; Modelling ; Moho ; Moho discontinuity ; Mountains ; Satellites ; Sedimentary basins ; Sedimentation & deposition ; Sediments ; Seismic data ; Seismic studies ; Seismology ; Tectonics ; Thickening ; Thickness ; Three dimensional models ; Topography ; Workflow</subject><ispartof>Solid earth (Göttingen), 2022-03, Vol.13 (2), p.431-448</ispartof><rights>COPYRIGHT 2022 Copernicus GmbH</rights><rights>2022. This work is published under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c474t-6a8f2451eb37a1dc8aa97ebcbc02bdae42cf66acf7cab662b34d9d4c204946e23</citedby><cites>FETCH-LOGICAL-c474t-6a8f2451eb37a1dc8aa97ebcbc02bdae42cf66acf7cab662b34d9d4c204946e23</cites><orcidid>0000-0001-7492-5338 ; 0000-0003-4155-9858</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2634694628/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2634694628?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,25753,27924,27925,37012,44590,75126</link.rule.ids></links><search><creatorcontrib>Ognev, Igor</creatorcontrib><creatorcontrib>Ebbing, Jörg</creatorcontrib><creatorcontrib>Haas, Peter</creatorcontrib><title>Crustal structure of the Volgo–Uralian subcraton revealed by inverse and forward gravity modelling</title><title>Solid earth (Göttingen)</title><description>Volgo-Uralia is a Neoarchaean easternmost part of the East European craton. Recent seismic studies of the Volgo-Uralian region provided new insights into the crustal structure of this area. In this study, we combine satellite gravity and seismic data in a common workflow to perform a complex study of Volgo-Uralian crustal structure, which is useful for further basin analysis of the area. In this light, a new crustal model of the Volgo-Uralian subcraton is presented from a step-wise approach: (1) inverse gravity modelling followed by (2) 3D forward gravity modelling.</description><subject>Analysis</subject><subject>Constraint modelling</subject><subject>Cratons</subject><subject>Crust</subject><subject>Crustal structure</subject><subject>Crustal thickness</subject><subject>Density</subject><subject>Earth</subject><subject>Earth science</subject><subject>Gravitational fields</subject><subject>Gravity anomalies</subject><subject>Gravity field</subject><subject>Mantle</subject><subject>Modelling</subject><subject>Moho</subject><subject>Moho discontinuity</subject><subject>Mountains</subject><subject>Satellites</subject><subject>Sedimentary basins</subject><subject>Sedimentation & deposition</subject><subject>Sediments</subject><subject>Seismic data</subject><subject>Seismic studies</subject><subject>Seismology</subject><subject>Tectonics</subject><subject>Thickening</subject><subject>Thickness</subject><subject>Three dimensional models</subject><subject>Topography</subject><subject>Workflow</subject><issn>1869-9529</issn><issn>1869-9510</issn><issn>1869-9529</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNptUk1v1DAQjRBIVKVXzpY4cUiJP-JsjtWKj5UqIQHlak3scfAqG5exs3Rv_Af-YX9JvRQBlToeaazRe2_G1quql7w5b3mv3iSsuayV5LVohHhSnfCV7uu-Ff3T_-7Pq7OUtk0J3YmulSeVW9OSMkwsZVpsXghZ9Cx_Q_Y1TmO8_fnrimAKMLO0DJYgx5kR7hEmdGw4sDDvkRIymB3zkX4AOTYS7EM-sF10OE1hHl9UzzxMCc_-1NPq6t3bL-sP9eXH95v1xWVtVadyrWHlhWo5DrID7uwKoO9wsINtxOAAlbBea7C-szBoLQapXO-UFY3qlUYhT6vNva6LsDXXFHZABxMhmN-NSKMBysFOaIRVrnXeFioo6cTQYqegPaYSwI9ar-61ril-XzBls40LzWV9I7RUukwUq3-osXyICbOPmcDuQrLmQvet6nqluoI6fwRVjsNdsHFGH0r_AeH1A0LBZLzJIywpmc3nT4-KW4opEfq_D-eNOXrDJDRcmuINc_SGvAM9iqzB</recordid><startdate>20220302</startdate><enddate>20220302</enddate><creator>Ognev, Igor</creator><creator>Ebbing, Jörg</creator><creator>Haas, Peter</creator><general>Copernicus GmbH</general><general>Copernicus Publications</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ISR</scope><scope>7SN</scope><scope>7ST</scope><scope>7UA</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>L7M</scope><scope>P5Z</scope><scope>P62</scope><scope>PCBAR</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>SOI</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0001-7492-5338</orcidid><orcidid>https://orcid.org/0000-0003-4155-9858</orcidid></search><sort><creationdate>20220302</creationdate><title>Crustal structure of the Volgo–Uralian subcraton revealed by inverse and forward gravity modelling</title><author>Ognev, Igor ; Ebbing, Jörg ; Haas, Peter</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c474t-6a8f2451eb37a1dc8aa97ebcbc02bdae42cf66acf7cab662b34d9d4c204946e23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Analysis</topic><topic>Constraint modelling</topic><topic>Cratons</topic><topic>Crust</topic><topic>Crustal structure</topic><topic>Crustal thickness</topic><topic>Density</topic><topic>Earth</topic><topic>Earth science</topic><topic>Gravitational fields</topic><topic>Gravity anomalies</topic><topic>Gravity field</topic><topic>Mantle</topic><topic>Modelling</topic><topic>Moho</topic><topic>Moho discontinuity</topic><topic>Mountains</topic><topic>Satellites</topic><topic>Sedimentary basins</topic><topic>Sedimentation & deposition</topic><topic>Sediments</topic><topic>Seismic data</topic><topic>Seismic studies</topic><topic>Seismology</topic><topic>Tectonics</topic><topic>Thickening</topic><topic>Thickness</topic><topic>Three dimensional models</topic><topic>Topography</topic><topic>Workflow</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ognev, Igor</creatorcontrib><creatorcontrib>Ebbing, Jörg</creatorcontrib><creatorcontrib>Haas, Peter</creatorcontrib><collection>CrossRef</collection><collection>Gale In Context: Science</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>ProQuest advanced technologies & aerospace journals</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environment Abstracts</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>Solid earth (Göttingen)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ognev, Igor</au><au>Ebbing, Jörg</au><au>Haas, Peter</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Crustal structure of the Volgo–Uralian subcraton revealed by inverse and forward gravity modelling</atitle><jtitle>Solid earth (Göttingen)</jtitle><date>2022-03-02</date><risdate>2022</risdate><volume>13</volume><issue>2</issue><spage>431</spage><epage>448</epage><pages>431-448</pages><issn>1869-9529</issn><issn>1869-9510</issn><eissn>1869-9529</eissn><abstract>Volgo-Uralia is a Neoarchaean easternmost part of the East European craton. Recent seismic studies of the Volgo-Uralian region provided new insights into the crustal structure of this area. In this study, we combine satellite gravity and seismic data in a common workflow to perform a complex study of Volgo-Uralian crustal structure, which is useful for further basin analysis of the area. In this light, a new crustal model of the Volgo-Uralian subcraton is presented from a step-wise approach: (1) inverse gravity modelling followed by (2) 3D forward gravity modelling.</abstract><cop>Gottingen</cop><pub>Copernicus GmbH</pub><doi>10.5194/se-13-431-2022</doi><tpages>18</tpages><orcidid>https://orcid.org/0000-0001-7492-5338</orcidid><orcidid>https://orcid.org/0000-0003-4155-9858</orcidid><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 1869-9529 |
ispartof | Solid earth (Göttingen), 2022-03, Vol.13 (2), p.431-448 |
issn | 1869-9529 1869-9510 1869-9529 |
language | eng |
recordid | cdi_doaj_primary_oai_doaj_org_article_2c4d5dfc049a43d2b5e74a54a5442a12 |
source | Publicly Available Content Database |
subjects | Analysis Constraint modelling Cratons Crust Crustal structure Crustal thickness Density Earth Earth science Gravitational fields Gravity anomalies Gravity field Mantle Modelling Moho Moho discontinuity Mountains Satellites Sedimentary basins Sedimentation & deposition Sediments Seismic data Seismic studies Seismology Tectonics Thickening Thickness Three dimensional models Topography Workflow |
title | Crustal structure of the Volgo–Uralian subcraton revealed by inverse and forward gravity modelling |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-01T00%3A17%3A16IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_doaj_&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Crustal%20structure%20of%20the%20Volgo%E2%80%93Uralian%20subcraton%20revealed%20by%20inverse%20and%20forward%20gravity%20modelling&rft.jtitle=Solid%20earth%20(G%C3%B6ttingen)&rft.au=Ognev,%20Igor&rft.date=2022-03-02&rft.volume=13&rft.issue=2&rft.spage=431&rft.epage=448&rft.pages=431-448&rft.issn=1869-9529&rft.eissn=1869-9529&rft_id=info:doi/10.5194/se-13-431-2022&rft_dat=%3Cgale_doaj_%3EA695479447%3C/gale_doaj_%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c474t-6a8f2451eb37a1dc8aa97ebcbc02bdae42cf66acf7cab662b34d9d4c204946e23%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2634694628&rft_id=info:pmid/&rft_galeid=A695479447&rfr_iscdi=true |