scholarly journals Piecemeal Delamination of Thickened Lithosphere Triggered Pulsed Magmatism and Mineralization during Late Mesozoic Intracontinental Orogeny in East Asia

2021 ◽  
Vol 95 (S1) ◽  
pp. 112-114
Author(s):  
Yueqiao ZHANG ◽  
Shuwen DONG ◽  
Jianhua LI ◽  
Erkang QIU
2018 ◽  
Vol 61 (12) ◽  
pp. 1888-1909 ◽  
Author(s):  
Shuwen Dong ◽  
Yueqiao Zhang ◽  
Hailong Li ◽  
Wei Shi ◽  
Huaimin Xue ◽  
...  

2019 ◽  
Vol 110 ◽  
pp. 539-564 ◽  
Author(s):  
Zhi-Xin Guo ◽  
Yong-Tai Yang ◽  
Xian-Zheng Zhao ◽  
Wei-Ning Dan ◽  
Xin Wang ◽  
...  

2021 ◽  
Vol 17 (8) ◽  
pp. 20210212
Author(s):  
Kazunori Yamahira ◽  
Satoshi Ansai ◽  
Ryo Kakioka ◽  
Hajime Yaguchi ◽  
Takeshi Kon ◽  
...  

The Indian subcontinent has an origin geologically different from Eurasia, but many terrestrial animal and plant species on it have congeneric or sister species in other parts of Asia, especially in the Southeast. This faunal and floral similarity between India and Southeast Asia is explained by either of the two biogeographic scenarios, ‘into-India’ or ‘out-of-India’. Phylogenies based on complete mitochondrial genomes and five nuclear genes were undertaken for ricefishes (Adrianichthyidae) to examine which of these two biogeographic scenarios fits better. We found that Oryzias setnai , the only adrianichthyid distributed in and endemic to the Western Ghats, a mountain range running parallel to the western coast of the Indian subcontinent, is sister to all other adrianichthyids from eastern India and Southeast–East Asia. Divergence time estimates and ancestral area reconstructions reveal that this western Indian species diverged in the late Mesozoic during the northward drift of the Indian subcontinent. These findings indicate that adrianichthyids dispersed eastward ‘out-of-India’ after the collision of the Indian subcontinent with Eurasia, and subsequently diversified in Southeast–East Asia. A review of geographic distributions of ‘out-of-India’ taxa reveals that they may have largely fuelled or modified the biodiversity of Eurasia.


2007 ◽  
Vol 42 (3-4) ◽  
pp. 391-413 ◽  
Author(s):  
Chen Peiji ◽  
Li Gang ◽  
David J. Batten
Keyword(s):  

2019 ◽  
pp. 60-77
Author(s):  
V. V. Yarmolyuk ◽  
A. V. Nikiforov ◽  
A. M. Kozlovsky ◽  
E. A. Kudryashova

The Late Mesozoic igneous province of East Asia in connection with global geological events is considered. The main structure-forming events and the largest magmatic productivity of the province coincided with the peak of widely manifested plume activity in the Early Cretaceous. A geodynamic model of the magmatic province formation is proposed, relating development of the province with the complex geodynamic setting for the interaction of the convergent boundary with the hot mantle field. The Pacific marginal magmatic belt was formed in front zone of convergence where accretion of terranes occurred with prevalence of supersubduction magma-forming mechanisms. In the western part of the province outside of convergence zone an intraplate volcanic areas were formed due to activity of small mantle plumes.


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