Linking deeply-sourced volatile emissions to plateau growth dynamics in southeastern Tibetan Plateau
Autor: | Cong-Qiang Liu, Zhihui Cheng, Zhengfu Guo, Lihong Zhang, Ai-Ti Chen, Yunchao Lang, Si-Liang Li, Zhongping Li, Guodong Zheng, Yuji Sano, Ying Li, Maoliang Zhang, Peter H. Barry, Sæmundur A. Halldórsson, Sheng Xu, Liwu Li |
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Jazyk: | angličtina |
Rok vydání: | 2021 |
Předmět: |
geography
Multidisciplinary Plateau geography.geographical_feature_category 010504 meteorology & atmospheric sciences Earth science Science Tectonics General Physics and Astronomy Context (language use) Geology General Chemistry Geodynamics Fault (geology) 010502 geochemistry & geophysics 01 natural sciences General Biochemistry Genetics and Molecular Biology Mantle (geology) Article Geochemistry 0105 earth and related environmental sciences |
Zdroj: | Nature Communications, Vol 12, Iss 1, Pp 1-10 (2021) Nature Communications |
ISSN: | 2041-1723 |
Popis: | The episodic growth of high-elevation orogenic plateaux is controlled by a series of geodynamic processes. However, determining the underlying mechanisms that drive plateau growth dynamics over geological history and constraining the depths at which growth originates, remains challenging. Here we present He-CO2-N2 systematics of hydrothermal fluids that reveal the existence of a lithospheric-scale fault system in the southeastern Tibetan Plateau, whereby multi-stage plateau growth occurred in the geological past and continues to the present. He isotopes provide unambiguous evidence for the involvement of mantle-scale dynamics in lateral expansion and localized surface uplift of the Tibetan Plateau. The excellent correlation between 3He/4He values and strain rates, along the strike of Indian indentation into Asia, suggests non-uniform distribution of stresses between the plateau boundary and interior, which modulate southeastward growth of the Tibetan Plateau within the context of India-Asia convergence. Our results demonstrate that deeply-sourced volatile geochemistry can be used to constrain deep dynamic processes involved in orogenic plateau growth. Deeply-sourced volatiles are releasing from orogenic plateau regions, providing windows to plateau growth dynamics occurring at variable depths. Here the authors show that mantle-derived volatiles reveal the involvement of mantle dynamics in southeastward growth of the Tibetan Plateau. |
Databáze: | OpenAIRE |
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