Illite K‐Ar Dating of the Leibo Fault Zone, Southeastern Margin of the Tibetan Plateau: Implications for the Quasi‐Synchronous Far‐Field Tectonic Response to the India‐Asia Collision

Abstract Whether tectonic strain from the early stage India‐Asia collision has synchronously affected the far‐field margin of the Tibetan Plateau is crucial for understanding plateau deformation and growth processes. However, direct evidence for early far‐field deformation remains scarce. Utilizing...

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Main Authors: Yuanhai Shu, Xuhua Shi, Samuel Haines, Hanlin Chen, Yong Zheng, Kongyang Zhu, Rong Yang, Haibing Li, Zhuona Bai, Jinhan Wang, Shufeng Yang
Format: Article
Language:English
Published: Wiley 2024-03-01
Series:Geophysical Research Letters
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Online Access:https://doi.org/10.1029/2023GL108027
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author Yuanhai Shu
Xuhua Shi
Samuel Haines
Hanlin Chen
Yong Zheng
Kongyang Zhu
Rong Yang
Haibing Li
Zhuona Bai
Jinhan Wang
Shufeng Yang
author_facet Yuanhai Shu
Xuhua Shi
Samuel Haines
Hanlin Chen
Yong Zheng
Kongyang Zhu
Rong Yang
Haibing Li
Zhuona Bai
Jinhan Wang
Shufeng Yang
author_sort Yuanhai Shu
collection DOAJ
description Abstract Whether tectonic strain from the early stage India‐Asia collision has synchronously affected the far‐field margin of the Tibetan Plateau is crucial for understanding plateau deformation and growth processes. However, direct evidence for early far‐field deformation remains scarce. Utilizing illite K‐Ar dating of three fault gouge samples, we established the faulting history of the Leibo fault zone (LFZ) at the southeastern margin of the Tibetan Plateau (SEMTP). Consistent authigenic illite ages of 52 ± 2, 54 ± 12 and 55 ± 6 Ma suggest the reactivated thrust faulting of the LFZ in the Early Cenozoic. Positioned ∼700 km east of the collisional boundary and at the intersection of three blocks with distinct lithospheric rheology in strength/viscosity, this event suggests a quasi‐synchronous far‐field tectonic response in the SEMTP to the India‐Asia collision.
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publishDate 2024-03-01
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series Geophysical Research Letters
spelling doaj-art-d594bbd1d1194b4cb2aea701e49a64302025-08-20T02:31:37ZengWileyGeophysical Research Letters0094-82761944-80072024-03-01516n/an/a10.1029/2023GL108027Illite K‐Ar Dating of the Leibo Fault Zone, Southeastern Margin of the Tibetan Plateau: Implications for the Quasi‐Synchronous Far‐Field Tectonic Response to the India‐Asia CollisionYuanhai Shu0Xuhua Shi1Samuel Haines2Hanlin Chen3Yong Zheng4Kongyang Zhu5Rong Yang6Haibing Li7Zhuona Bai8Jinhan Wang9Shufeng Yang10Key Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province School of Earth Sciences Zhejiang University Hangzhou ChinaKey Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province School of Earth Sciences Zhejiang University Hangzhou ChinaDanish Offshore Technology Centre Kongens Lyngby DenmarkKey Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province School of Earth Sciences Zhejiang University Hangzhou ChinaInstitute of Geology Chinese Academy of Geological Sciences Beijing ChinaKey Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province School of Earth Sciences Zhejiang University Hangzhou ChinaKey Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province School of Earth Sciences Zhejiang University Hangzhou ChinaInstitute of Geology Chinese Academy of Geological Sciences Beijing ChinaKey Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province School of Earth Sciences Zhejiang University Hangzhou ChinaKey Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province School of Earth Sciences Zhejiang University Hangzhou ChinaKey Laboratory of Geoscience Big Data and Deep Resource of Zhejiang Province School of Earth Sciences Zhejiang University Hangzhou ChinaAbstract Whether tectonic strain from the early stage India‐Asia collision has synchronously affected the far‐field margin of the Tibetan Plateau is crucial for understanding plateau deformation and growth processes. However, direct evidence for early far‐field deformation remains scarce. Utilizing illite K‐Ar dating of three fault gouge samples, we established the faulting history of the Leibo fault zone (LFZ) at the southeastern margin of the Tibetan Plateau (SEMTP). Consistent authigenic illite ages of 52 ± 2, 54 ± 12 and 55 ± 6 Ma suggest the reactivated thrust faulting of the LFZ in the Early Cenozoic. Positioned ∼700 km east of the collisional boundary and at the intersection of three blocks with distinct lithospheric rheology in strength/viscosity, this event suggests a quasi‐synchronous far‐field tectonic response in the SEMTP to the India‐Asia collision.https://doi.org/10.1029/2023GL108027Leibo fault zonefault gougeillite K‐Ar datingquasi‐synchronous far‐field tectonic responsesoutheastern margin of the Tibetan PlateauIndia‐Asia collision
spellingShingle Yuanhai Shu
Xuhua Shi
Samuel Haines
Hanlin Chen
Yong Zheng
Kongyang Zhu
Rong Yang
Haibing Li
Zhuona Bai
Jinhan Wang
Shufeng Yang
Illite K‐Ar Dating of the Leibo Fault Zone, Southeastern Margin of the Tibetan Plateau: Implications for the Quasi‐Synchronous Far‐Field Tectonic Response to the India‐Asia Collision
Geophysical Research Letters
Leibo fault zone
fault gouge
illite K‐Ar dating
quasi‐synchronous far‐field tectonic response
southeastern margin of the Tibetan Plateau
India‐Asia collision
title Illite K‐Ar Dating of the Leibo Fault Zone, Southeastern Margin of the Tibetan Plateau: Implications for the Quasi‐Synchronous Far‐Field Tectonic Response to the India‐Asia Collision
title_full Illite K‐Ar Dating of the Leibo Fault Zone, Southeastern Margin of the Tibetan Plateau: Implications for the Quasi‐Synchronous Far‐Field Tectonic Response to the India‐Asia Collision
title_fullStr Illite K‐Ar Dating of the Leibo Fault Zone, Southeastern Margin of the Tibetan Plateau: Implications for the Quasi‐Synchronous Far‐Field Tectonic Response to the India‐Asia Collision
title_full_unstemmed Illite K‐Ar Dating of the Leibo Fault Zone, Southeastern Margin of the Tibetan Plateau: Implications for the Quasi‐Synchronous Far‐Field Tectonic Response to the India‐Asia Collision
title_short Illite K‐Ar Dating of the Leibo Fault Zone, Southeastern Margin of the Tibetan Plateau: Implications for the Quasi‐Synchronous Far‐Field Tectonic Response to the India‐Asia Collision
title_sort illite k ar dating of the leibo fault zone southeastern margin of the tibetan plateau implications for the quasi synchronous far field tectonic response to the india asia collision
topic Leibo fault zone
fault gouge
illite K‐Ar dating
quasi‐synchronous far‐field tectonic response
southeastern margin of the Tibetan Plateau
India‐Asia collision
url https://doi.org/10.1029/2023GL108027
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