魏晓椿

With Certificate of Graduation for Doctorate Study /Lecturer

魏晓椿,博士,现任长江大学地球科学学院特任副教授,硕士生导师。主持或参与国家自然科学基金、中国科学院战略性先导科技专项等多项。重点关注青藏高原的隆升过程、机制及其资源环境效应。 目前以第一作者和通讯作者在PNAS(美国科学院院刊)、Tectonics、GSA Bulletin和Tectonophysics等期刊发表论文多篇。以合作者身份在EPSL、JGR: Solid Earth、GSA Bulletin、Palaeogeography  Pa...

Paper Publications

Timing and Kinematics of late Cenozoic Strike-slip Faults in the Western Tibetan Plateau: New Constraints from Provenance Analysis and Detrital Thermochronology

Release time:
2025-03-28
Hits:
DOI number:
10.1016/j.tecto.2024.230353
Journal:
Tectonophysics
Abstract:
The activities of the three large strike-slip fault systems — the Karakoram, the Karakax, and the Longmu Co-Guozha Co faults — located in the western Tibetan Plateau have induced the intense exhumation of the Karakoram and the southern Western Kunlun ranges. However, the histories of these faults remain debated or loosely constrained, partly due to the restricted access to bedrock samples and associated comprehensive analyses. The application of detrital provenance analysis and detrital thermochronology to sediments can provide valuable information on the locations, crystallization timing, and exhumation of the source terranes of the sediments, thereby shedding light on tectonic histories. This study utilizes modern fluvial sand to obtain exhumation information on the Karakoram and the southern Western Kunlun ranges and to reconstruct the history of the major faults. We achieve this through provenance analysis (heavy-mineral analysis and detrital zircon UPb dating) and detrital apatite fission-track dating. Our results reveal widespread Paleogene rock exhumation across the western Tibetan Plateau and focused mid-Miocene (ca. 15–12 Ma) exhumation along the Karakoram and the southern Western Kunlun ranges. Moreover, the Karakoram Range experienced renewed exhumation at ca. 7 Ma. Through an integration of our results and regional geological evidence, we suggest that the focused mid-Miocene exhumation reflects the initiation of the Karakoram and the Karakax faults; the subsequent ca. 7 Ma exhumation episode of the Karakoram Range indicates a regional kinematic reorganization due to the initiation of the Longmu Co-Guozha Co Fault. We propose that middle and late Miocene strike-slip faulting in the western Tibetan Plateau was driven by oblique underthrusting of the Indian lithosphere.
Co-author:
Yang Rong, Wang Ping, Li Shanying, Shi Xuhua, Ge Jin
First Author:
Wei Xiaochun
Indexed by:
期刊文章
Correspondence Author:
Chen Hanlin
Volume:
882
Issue:
Page Number:
230353
ISSN No.:
0040-1951
Date of Publication:
2024-05-01