Early Permian mafic dikes in the Nagqu area, central Tibet, China, associated with embryonic oceanic crust of the Meso-Tethys Ocean

2017 ◽  
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Ren-Deng Shi ◽  
Wei-Ming Fan ◽  
Xiao-Han Gong ◽  
Kang Wu
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Bin Wang ◽  
Chao-Ming Xie ◽  
Yong-sheng Dong ◽  
Jian-Jun Fan ◽  
Yun-Peng Yu ◽  
...  

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Paul Kapp ◽  
George E. Gehrels ◽  
Jeff D. Vervoort ◽  
Lin Ding

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Hongqi Chen ◽  
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pp. 1670-1686 ◽  
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Yong-Sheng Dong ◽  
Qiang Wang ◽  
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Chunfu Zhang ◽  
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Bizhan Yousefi Yegane ◽  
A.J. van Loon Tom ◽  
Sakine Arefi Fard ◽  
Mohammad Mehdi Farahpour ◽  
Safoora Yasbolaghi Sharahi

Abstract A transgression of the Tethys Ocean occurred in east central Iran, like in other areas of the Tethys Ocean, around the Yakhtashian/Bolorian (regional chronostratigraphical units corresponding with the Artinskian/Kungurian of the Early Permian) transition. This led to the development of a carbonate platform that is represented in the Shirgesht area on the northern part of the Tabas Block by the Bagh-e-Vang Formation, which constitutes the only known sedimentary unit from the late Early Permian in Iran. Field data and thin-section analysis indicate deposition on a carbonate ramp with barriers separating a lagoonal area with intertidal mud flats from the open-marine environment. The overall transgressive development is indicated by the presence of open-marine sediments on top of the barrier and lagoonal sediments.


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