Three‐dimensional electrical structure of the crust and upper mantle in Ordos Block and adjacent area: Evidence of regional lithospheric modification

Abstract Long‐period magnetotelluric (MT) data from project SINOPROBE were acquired and modeled, using three‐dimensional (3D) MT inversion, to study the electrical structure of Ordos Block, a component of the North China Craton. For the first time, a high‐resolution 3D resistivity model of the litho...

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Main Authors: Hao Dong, Wenbo Wei, Gaofeng Ye, Sheng Jin, Alan G. Jones, Jianen Jing, Letian Zhang, Chengliang Xie, Fan Zhang, Hui Wang
Format: Article
Language:English
Published: Wiley 2014-06-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1002/2014GC005270
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author Hao Dong
Wenbo Wei
Gaofeng Ye
Sheng Jin
Alan G. Jones
Jianen Jing
Letian Zhang
Chengliang Xie
Fan Zhang
Hui Wang
author_facet Hao Dong
Wenbo Wei
Gaofeng Ye
Sheng Jin
Alan G. Jones
Jianen Jing
Letian Zhang
Chengliang Xie
Fan Zhang
Hui Wang
author_sort Hao Dong
collection DOAJ
description Abstract Long‐period magnetotelluric (MT) data from project SINOPROBE were acquired and modeled, using three‐dimensional (3D) MT inversion, to study the electrical structure of Ordos Block, a component of the North China Craton. For the first time, a high‐resolution 3D resistivity model of the lithosphere is defined for the region. Contrary to what would be expected for a stable cratonic block, a prominent lithospheric conductive complex is revealed extending from the upper mantle to the mid‐to‐lower crust beneath the northern part of Ordos. Correlating well with results of seismic studies, the evidence from our independent magnetotelluric data supports regional modification of the lithosphere under the north Ordos and lithosphere thinning beneath Hetao Graben. The abnormally conductive structure may result from upwelling of mantle material in mid‐to‐late Mesozoic beneath the northern margin of the Ordos block.
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publisher Wiley
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series Geochemistry, Geophysics, Geosystems
spelling doaj-art-75fef418554b4ddf9f957c36096202cd2025-08-20T02:35:19ZengWileyGeochemistry, Geophysics, Geosystems1525-20272014-06-011562414242510.1002/2014GC005270Three‐dimensional electrical structure of the crust and upper mantle in Ordos Block and adjacent area: Evidence of regional lithospheric modificationHao Dong0Wenbo Wei1Gaofeng Ye2Sheng Jin3Alan G. Jones4Jianen Jing5Letian Zhang6Chengliang Xie7Fan Zhang8Hui Wang9School of Geophysics and Information TechnologyChina University of GeosciencesBeijing ChinaSchool of Geophysics and Information TechnologyChina University of GeosciencesBeijing ChinaSchool of Geophysics and Information TechnologyChina University of GeosciencesBeijing ChinaSchool of Geophysics and Information TechnologyChina University of GeosciencesBeijing ChinaDublin Institute for Advanced StudiesDublin IrelandSchool of Geophysics and Information TechnologyChina University of GeosciencesBeijing ChinaSchool of Geophysics and Information TechnologyChina University of GeosciencesBeijing ChinaSchool of Geophysics and Information TechnologyChina University of GeosciencesBeijing ChinaSchool of Geophysics and Information TechnologyChina University of GeosciencesBeijing ChinaSchool of Geophysics and Information TechnologyChina University of GeosciencesBeijing ChinaAbstract Long‐period magnetotelluric (MT) data from project SINOPROBE were acquired and modeled, using three‐dimensional (3D) MT inversion, to study the electrical structure of Ordos Block, a component of the North China Craton. For the first time, a high‐resolution 3D resistivity model of the lithosphere is defined for the region. Contrary to what would be expected for a stable cratonic block, a prominent lithospheric conductive complex is revealed extending from the upper mantle to the mid‐to‐lower crust beneath the northern part of Ordos. Correlating well with results of seismic studies, the evidence from our independent magnetotelluric data supports regional modification of the lithosphere under the north Ordos and lithosphere thinning beneath Hetao Graben. The abnormally conductive structure may result from upwelling of mantle material in mid‐to‐late Mesozoic beneath the northern margin of the Ordos block.https://doi.org/10.1002/2014GC005270lithosphere modificationmagnetotelluricsOrdos BlockSINOPROBENorth China
spellingShingle Hao Dong
Wenbo Wei
Gaofeng Ye
Sheng Jin
Alan G. Jones
Jianen Jing
Letian Zhang
Chengliang Xie
Fan Zhang
Hui Wang
Three‐dimensional electrical structure of the crust and upper mantle in Ordos Block and adjacent area: Evidence of regional lithospheric modification
Geochemistry, Geophysics, Geosystems
lithosphere modification
magnetotellurics
Ordos Block
SINOPROBE
North China
title Three‐dimensional electrical structure of the crust and upper mantle in Ordos Block and adjacent area: Evidence of regional lithospheric modification
title_full Three‐dimensional electrical structure of the crust and upper mantle in Ordos Block and adjacent area: Evidence of regional lithospheric modification
title_fullStr Three‐dimensional electrical structure of the crust and upper mantle in Ordos Block and adjacent area: Evidence of regional lithospheric modification
title_full_unstemmed Three‐dimensional electrical structure of the crust and upper mantle in Ordos Block and adjacent area: Evidence of regional lithospheric modification
title_short Three‐dimensional electrical structure of the crust and upper mantle in Ordos Block and adjacent area: Evidence of regional lithospheric modification
title_sort three dimensional electrical structure of the crust and upper mantle in ordos block and adjacent area evidence of regional lithospheric modification
topic lithosphere modification
magnetotellurics
Ordos Block
SINOPROBE
North China
url https://doi.org/10.1002/2014GC005270
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