Provenance and sedimentary evolution from the Middle Permian to Early Triassic around the Bogda Mountain, NW China: A tectonic inversion responding to the consolidation of Pangea

2020 ◽  
Vol 114 ◽  
pp. 104169 ◽  
Author(s):  
Yanqing Shi ◽  
Hancheng Ji ◽  
Jingwei Yu ◽  
Pengfei Xiang ◽  
Zhibo Yang ◽  
...  
2012 ◽  
Vol 43 (1) ◽  
pp. 130-144 ◽  
Author(s):  
Aymon Baud ◽  
Sylvain Richoz ◽  
Benoit Beauchamp ◽  
Fabrice Cordey ◽  
Stephen Grasby ◽  
...  

2018 ◽  
Vol 164 ◽  
pp. 83-103 ◽  
Author(s):  
Namık Aysal ◽  
Sabah Yılmaz Şahin ◽  
Yıldırım Güngör ◽  
Irena Peytcheva ◽  
Sinan Öngen

2020 ◽  
Author(s):  
Kaibo Shi ◽  
Bo Liu ◽  
Weimin Jiang ◽  
Jinxing Yu ◽  
Yue Kong ◽  
...  

2007 ◽  
Vol 243 (3-4) ◽  
pp. 394-411 ◽  
Author(s):  
Thomas Galfetti ◽  
Hugo Bucher ◽  
Arnaud Brayard ◽  
Peter A. Hochuli ◽  
Helmut Weissert ◽  
...  

1979 ◽  
Vol 116 (5) ◽  
pp. 385-392 ◽  
Author(s):  
J. B. Waterhouse

SummaryAlthough the ammonoid Durvilleoceras is apparently very close in its morphology to early Triassic genera, it comes from a formation that underlies formations with early Triassic and late Permian faunas, and appears to be of late Middle Permian age. New occurrences of the ammonoid support this thesis. Conjecturally, the genus may have inhabited deep cold waters of the southern hemisphere during the Permian Period, before giving rise to genera found in shelf deposits of the early Triassic. Alternatively, if really Triassic in age, Durvilleoceras indicates a major low-angle thrust, previously unsuspected, that has repeated Triassic sequences for a length of over 450 km before disruption by the Alpine Fault. No evidence is yet known to support this alternative.


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