NDLI: Structural framework and its evolution in Chasang area of Qiangtang Basin in northern Tibetan

Content Provider	Springer Nature Link
Author	Liu, Chiyang Yang, Xingke Ren, Zhanli Lai, Shaocong Chen, Gang Zhao, Hongge Wei, Yongpei Zheng, Menglin Wang, Chengshan
Copyright Year	2001
Abstract	Through comprehensive research on the various geophysical and geological data acquired recently, we consider that the Chasang area in the western uplift of Qiangtang is a huge south-dipping block which is overlapped by several east-west trending blocks rather than a simple and palaeo-doming existing for a long time. The structural and geophysical features of the area, which only alone limited between Shuanghu and Rongma districts, are of no regional significance. Their development is closely related with the approximately south-north trending transform faults developed during the Mesozoic era on the east and west sides of the area and their later continuous movement. The compressing, overlapping and uplifting of the Chasang area began at the stage of reversing of the Qiangtang Basin during the Lower Cretaceous, which is in direct relation with Bangonghu-Dingqing limited ocean’s closure and the convergence of the neighboring blocks. The compression and overlapping of the area have further developed and reformed since the Eocene because of the continuing collision and pushing of the Indian Plate to the north.
Starting Page	18
Ending Page	26
Page Count	9
File Format	PDF
ISSN	10069313
Journal	Science in China Series D: Earth Sciences
Volume Number	44
Issue Number	1
e-ISSN	18622801
Language	English
Publisher	Science in China Press
Publisher Date	2001-01-01
Publisher Place	Beijing
Access Restriction	Subscribed
Subject Keyword	Qinghai-Tibetan Plateau Qiangtang basin Chasang area structure framework compressing and shortening napping and overlapping transverse transform fault Geosciences
Content Type	Text
Resource Type	Article
Subject	Earth and Planetary Sciences

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