Sedimentation and mineralization of the Late Paleozoic extensional basin in the western Kunlun Mountains, China
In the western Kunlun Mountain region, due to the convergence of the Paleotethys Ocean in the Late Paleozoic, through northward subduction towards the West Kunlun Block, forming the Kangxiwa–Waqia arc magmatism and back-arc extensional basins, including the Tamu–Kalangu and Oytag–Kurliang basins. Th...
Main Authors: | , , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Elsevier
2021-06-01
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Series: | Solid Earth Sciences |
Subjects: | |
Online Access: | http://www.sciencedirect.com/science/article/pii/S2451912X21000040 |