Transition from non-adakitic rocks to adakitic rocks in the southern Lhasa subterrane: Implications for progressive crustal thickening and tectonic evolution during the Early Cenozoic-Reference-Cited by-同舟云学术

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Transition from non-adakitic rocks to adakitic rocks in the southern Lhasa subterrane: Implications for progressive crustal thickening and tectonic evolution during the Early Cenozoic

Published:2024-03 Issue: Volume:262 Page:105995
ISSN:1367-9120
Container-title:Journal of Asian Earth Sciences
language:en
Short-container-title:Journal of Asian Earth Sciences

Author:

Yan Haoyu^ORCID,Xu Zhiqin,Long Xiaoping,Li Jie,Shu Chutian,Gou Longlong,Wu Bin

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference162 articles.

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

2. The genesis of intermediate and silicic magmas in deep crustal hot zones;Annen;J. Petrol.,2006

3. Generation of sodium-rich magmas from newly underplated basaltic crust;Atherton;Nature,1993

4. The volcanic-plutonic connection as a stage for understanding crustal magmatism;Bachmann;J. Volcanol. Geoth. Res.,2007

5. Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholith, California: nature, origin, and relations with the hosts;Barbarin;Lithos,2005

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