Evolution of the Neo-Tethys traced by Late Triassic to Early Cretaceous marine remnants in the eastern segment of the Yarlung-Tsangpo suture zone, southern Tibet-Reference-Cited by-同舟云学术

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Evolution of the Neo-Tethys traced by Late Triassic to Early Cretaceous marine remnants in the eastern segment of the Yarlung-Tsangpo suture zone, southern Tibet

Published:2024-04 Issue: Volume:265 Page:106090
ISSN:1367-9120
Container-title:Journal of Asian Earth Sciences
language:en
Short-container-title:Journal of Asian Earth Sciences

Author:

He Zhihao,Li Xin,Li Yalin,Matsuoka Atsushi,Luo Hui,Cui Xiaohui,Cheng Jianbo

Publisher

Elsevier BV

Reference69 articles.

1. Hydrothermal chert and associated siliceous rocks from the northern Pacific: their geological significance as indication of ocean ridge activity;Adachi;Sedimentary. Geol.,1986

2. Geochemical constraints on the depositional setting of Paleozoic chert from the New England Orogen, NSW, eastern Australia;Aitchison;Mar. Geol.,1990

3. Remnants of a Cretaceous intra-oceanic subduction system within the Yarlung-Zangbo suture (southern Tibet);Aitchison;Earth Planet. Sci. Lett.,2000

4. Stratigraphic and sedimentological constraints on the age and tectonic evolution of the Neotethyan ophiolites along the Yarlung Tsangpo suture zone;Aitchison;Tibet. Geol Soc Spec Publ.,2003

5. When and where did India and Asia collide?;Aitchison;J. Geophys. Res.,2007

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