A late Permian–Triassic trench‐slope basin in the Central Qiangtang Metamorphic Belt, Northern Tibet: stratigraphy, sedimentology, syndepositional deformation and tectonic implications

2021 ◽  
Author(s):  
Xiao Liang ◽  
Genhou Wang ◽  
Jinhan Gao ◽  
Haishui Jiang ◽  
Guoli Yuan ◽  
...  



Author(s):  
G. DRAPER ◽  
R. R. HARDING ◽  
W. T. HORSFIELD ◽  
A. W. KEMP ◽  
A. E. TRESHAM


2000 ◽  
Vol 173 (1) ◽  
pp. 83-96 ◽  
Author(s):  
Demir Altiner ◽  
Sevinç Özkan-Altiner ◽  
Ali Koçyiğit


2015 ◽  
Vol 100 ◽  
pp. 132-144 ◽  
Author(s):  
Qing-yuan Jiang ◽  
Cai Li ◽  
Li Su ◽  
Pei-yuan Hu ◽  
Chao-ming Xie ◽  
...  


2005 ◽  
Vol 47 (4) ◽  
pp. 344-370 ◽  
Author(s):  
S. W. Kim ◽  
C. W. Oh ◽  
H. Hyodo ◽  
T. Itaya ◽  
J. G. Liou


2015 ◽  
Vol 153 (3) ◽  
pp. 537-543 ◽  
Author(s):  
YI-CHUN ZHANG ◽  
SHU-ZHONG SHEN ◽  
QING-GUO ZHAI ◽  
YU-JIE ZHANG ◽  
DONG-XUN YUAN

AbstractThe Qiangtang Metamorphic Belt (QMB) was considered to have either formed in situ by amalgmation of the North and South Qiangtang blocks or been underthrust from the Jinsha suture and exhumed in the interior of a single ‘Qiangtang Block’. A new Sphaeroschwagerina fusuline fauna discovered in the Raggyorcaka Lake area supports the interpretation that the North and South Qiangtang blocks were separated by a wide ocean during Asselian (Early Permian) time, indicating that the QMB was formed by the suturing of the Palaeotethys Ocean along the Longmu Co-Shuanghu suture.



Sign in / Sign up

Export Citation Format

Share Document