A review on the magnetotelluric studies over the Central Asian Orogenic Belt—recent developments and future aspects
The Central Asian Orogenic Belt (CAOB) was originated from the subduction, closure, convergence, and post-collisional extension of the Paleo-Asian Ocean located between the North China Craton, Tarim Craton, and the Siberian Craton during the late Permian to early Triassic. The Magnetotelluric (MT) m...
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Frontiers Media S.A.
2025-01-01
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| Series: | Frontiers in Earth Science |
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| Online Access: | https://www.frontiersin.org/articles/10.3389/feart.2024.1526432/full |
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| author | Yifan Li Letian Zhang Letian Zhang Letian Zhang Sheng Jin Sheng Jin Lishui Zhou Qiyao Zong |
| author_facet | Yifan Li Letian Zhang Letian Zhang Letian Zhang Sheng Jin Sheng Jin Lishui Zhou Qiyao Zong |
| author_sort | Yifan Li |
| collection | DOAJ |
| description | The Central Asian Orogenic Belt (CAOB) was originated from the subduction, closure, convergence, and post-collisional extension of the Paleo-Asian Ocean located between the North China Craton, Tarim Craton, and the Siberian Craton during the late Permian to early Triassic. The Magnetotelluric (MT) method can detect the deep structure and properties of the orogenic belt, and further reveal the crust and mantle deformation mechanism and deep dynamic process inside the orogenic belt. In this paper, we summarize recent developments in the MT studies of the CAOB, including 2 MT studies that we recently conducted for the Beishan and Bainaimiao segments of the CAOB, which briefly describe the complex electrical structure of the crust and upper mantle, and provide valuable information for understanding its deep processes and continental dynamic mechanisms. Finally, we summarize the general characteristics of the lithospheric electrical structure and formation mechanism of low-resistivity zones, based on which we look forward to future MT studies. |
| format | Article |
| id | doaj-art-2852c0fd885c4d0d84ffcff5ca76c0ed |
| institution | Kabale University |
| issn | 2296-6463 |
| language | English |
| publishDate | 2025-01-01 |
| publisher | Frontiers Media S.A. |
| record_format | Article |
| series | Frontiers in Earth Science |
| spelling | doaj-art-2852c0fd885c4d0d84ffcff5ca76c0ed2025-01-20T07:20:13ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632025-01-011210.3389/feart.2024.15264321526432A review on the magnetotelluric studies over the Central Asian Orogenic Belt—recent developments and future aspectsYifan Li0Letian Zhang1Letian Zhang2Letian Zhang3Sheng Jin4Sheng Jin5Lishui Zhou6Qiyao Zong7School of Geophysics and Information Technology, China University of Geosciences (Beijing), Beijing, ChinaSchool of Geophysics and Information Technology, China University of Geosciences (Beijing), Beijing, ChinaState Key Laboratory of Geological Process and Mineral Resources, Beijing, ChinaKey Laboratory of Intraplate Volcanoes and Earthquakes, Ministry of Education, Beijing, ChinaSchool of Geophysics and Information Technology, China University of Geosciences (Beijing), Beijing, ChinaCollege of Earth Sciences, Hebei GEO University, Shijiazhuang, ChinaSchool of Geophysics and Information Technology, China University of Geosciences (Beijing), Beijing, ChinaSchool of Geophysics and Information Technology, China University of Geosciences (Beijing), Beijing, ChinaThe Central Asian Orogenic Belt (CAOB) was originated from the subduction, closure, convergence, and post-collisional extension of the Paleo-Asian Ocean located between the North China Craton, Tarim Craton, and the Siberian Craton during the late Permian to early Triassic. The Magnetotelluric (MT) method can detect the deep structure and properties of the orogenic belt, and further reveal the crust and mantle deformation mechanism and deep dynamic process inside the orogenic belt. In this paper, we summarize recent developments in the MT studies of the CAOB, including 2 MT studies that we recently conducted for the Beishan and Bainaimiao segments of the CAOB, which briefly describe the complex electrical structure of the crust and upper mantle, and provide valuable information for understanding its deep processes and continental dynamic mechanisms. Finally, we summarize the general characteristics of the lithospheric electrical structure and formation mechanism of low-resistivity zones, based on which we look forward to future MT studies.https://www.frontiersin.org/articles/10.3389/feart.2024.1526432/fullmagnetotelluricsCentral Asian Orogenic BeltPaleo-Asian Oceanlithospheric electrical structureformation mechanism of low-resistivity zones |
| spellingShingle | Yifan Li Letian Zhang Letian Zhang Letian Zhang Sheng Jin Sheng Jin Lishui Zhou Qiyao Zong A review on the magnetotelluric studies over the Central Asian Orogenic Belt—recent developments and future aspects Frontiers in Earth Science magnetotellurics Central Asian Orogenic Belt Paleo-Asian Ocean lithospheric electrical structure formation mechanism of low-resistivity zones |
| title | A review on the magnetotelluric studies over the Central Asian Orogenic Belt—recent developments and future aspects |
| title_full | A review on the magnetotelluric studies over the Central Asian Orogenic Belt—recent developments and future aspects |
| title_fullStr | A review on the magnetotelluric studies over the Central Asian Orogenic Belt—recent developments and future aspects |
| title_full_unstemmed | A review on the magnetotelluric studies over the Central Asian Orogenic Belt—recent developments and future aspects |
| title_short | A review on the magnetotelluric studies over the Central Asian Orogenic Belt—recent developments and future aspects |
| title_sort | review on the magnetotelluric studies over the central asian orogenic belt recent developments and future aspects |
| topic | magnetotellurics Central Asian Orogenic Belt Paleo-Asian Ocean lithospheric electrical structure formation mechanism of low-resistivity zones |
| url | https://www.frontiersin.org/articles/10.3389/feart.2024.1526432/full |
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