期刊
GONDWANA RESEARCH
卷 17, 期 1, 页码 135-144出版社
ELSEVIER
DOI: 10.1016/j.gr.2009.04.010
关键词
SHRIMP dating; Continental rift setting; Nadi Kangri volcanic rocks; Qiangtang basin, northern Tibet
资金
- National Natural Science Foundation of China [40702020]
- National Oil and Gas Special Project: Strategic investigation and Geological Survey on Tibet Oil and Gas Resources [XQ200406]
The Late Triassic Nadi Kangri volcanic rocks, with nearly EW trending outcrops within the Qiangtang basin, northern Xizang (Tibet), China, are composed mainly of acid tuff, dacite, rhyolite and minor basic volcanic rocks. There exists a significant depositional hiatus between the Nadi Kangri volcanic rocks and underlying strata. Therefore, the Nadi Kangri volcanic rocks represent a new evolution history of the Mesozoic Qiangtang basin. The magma emplacement age of the Nadi Kangri volcanic rocks in the Geladaindong area is 220.4 +/- 2.3 Ma, representing the onset of the Mesozoic Qiangtang basin. The Nadi Kangri basalts have high Nb/Zr (0.049-0.058), Ta/Hf (0.12-0.15) and Zr/Y (4.95-6.01) ratios. In the tectonic discrimination diagrams, such as Zr vs. Zr/Y and Th/Hf vs. Ta/Hf, the Nadi Kangri basaltic rocks mostly plot in the within-plate setting field. The geological background and the geochemical characteristics suggest that the Nadi Kangri volcanic rocks were formed in a continental rift setting. Crown Copyright (C) 2009 Published by Elsevier B.V. on behalf of International Association for Gondwana Research. All rights reserved.
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