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

Northward expansion of the West Kunlun orogenic belt during the Cenozoic and its implications for the evolution of the northwest Tibetan Plateau: Constraints from sediment dispersal patterns in the Buya Basin, China

Release time:
2025-03-28
Hits:
DOI number:
10.1016/j.palaeo.2024.112255
Journal:
Palaeogeography, Palaeoclimatology, Palaeoecology
Abstract:
The West Kunlun orogenic belt, which defines the northwestern margin of the Tibetan Plateau, holds important information on plateau growth. Despite its significance, views about its uplift history continues to be under debate, with two competing hypotheses involving episodic uplift or northward expansion, related to a fixed or movable plateau boundary, respectively. The Buya Basin, a small basin located between the North and South Kunlun terranes, is key to understanding the Cenozoic uplift history of the West Kunlun orogenic belt. In this study, we conducted sedimentary and detrital zircon UPb geochronological analyses on the Cenozoic sediments of the Buya Basin. According to the findings of the sedimentary investigation, the Cenozoic strata of the basin generally show gradual changes from low- to high-energy deposition interrupted by a reverse trend in the Anjuan Formation. Moreover, the detrital zircon UPb geochronological results indicate that the Buya Basin received sediments initially from the Songpan–Ganzi and South Kunlun terranes during the deposition of the Keziluoyi to Pakabulake formations and then from the South and North Kunlun terranes during the deposition of the Artux Formation. This change in sediment dispersal patterns demonstrates that the uplift of the West Kunlun orogenic belt has expanded northwards to the North Kunlun terrane, which suggests that the northwestern boundary of the Tibetan Plateau has been a northward-moving feature in the context of India–Eurasia convergence. Along with previous studies, we suggest that the northward expansion of the northwest Tibetan Plateau is accommodated by decoupling deformation along the southern Tarim Basin, with northward thrusting of the foreland fold-and-thrust belts in the upper crust and southward underthrusting in the lower plate.
Co-author:
Li Chunyang, Wei Xiaochun, Qu Yang, An Kaixuan, Chen Cai, Yang Xianzhang, Li Yong, Zhang Liang, Shang Jiangwei, Li Li, Huang Jialun, Lei Yuwei, Wang Cong, Chen Hanlin, Jiang Lin, Su Nan, Wang Lining
First Author:
Liang Shujun
Indexed by:
期刊文章
Correspondence Author:
Lin Xiubin
Volume:
647
Issue:
Page Number:
112255
ISSN No.:
0031-0182
Date of Publication:
2024-08-01