Sandstone provenance and tectonic evolution of the Xiukang Mélange from Neotethyan subduction to India–Asia collision (Yarlung-Zangbo suture, south Tibet)
Author:
Funder
NSFC Project
CAS Strategic Priority Research Program
MOST 973 Project
Publisher
Elsevier BV
Subject
Geology
Reference102 articles.
1. Evidence for Early (>44Ma) Himalayan crustal thickening, Tethyan Himalaya, southeastern Tibet;Aikman;Earth and Planetary Science Letters,2008
2. When and where did India and Asia collide?;Aitchison;Journal of Geophysical Research - Solid Earth,2007
3. Remnants of a Cretaceous intra-oceanic subduction system within the Yarlung-Zangbo suture (southern Tibet);Aitchison;Earth and Planetary Science Letters,2000
4. Detrital zircon U–Pb ages along the Yarlung-Tsangpo suture zone, Tibet: implications for oblique convergence and collision between India and Asia;Aitchison;Gondwana Research,2011
5. Architecture of the Chugach accretionary complex as revealed by detrital zircon ages and lithologic variations: evidence for Mesozoic subduction erosion in south-central Alaska;Amato;Geological Society of America Bulletin,2013
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