Cenozoic volcanism and intraplate subduction at the northern margin of the Tibetan Plateau
- 1 April 1991
- journal article
- research article
- Published by Springer Science and Business Media LLC in Chinese Journal of Geochemistry
- Vol. 10 (2), 140-152
- https://doi.org/10.1007/bf02837714
Abstract
Developed in the Mt. Kunlun orogenic belt at the northern margin of the Tibetan Plateau is an active Cenozoic volcanic zone which is more than 1000km in length and some ten to hundred kilometers in width. It extends east-westwards and is roughly parallel to the strike of Mt. Kunlun. The Cenozoic volcanic rocks are divided into the northern (N-) and southern (S-) subzones. Eruptions of volcanic lavas in the S-subzone are related to an initial rift zone within the north Qiangtang terrane, but the volcanic rocks in the N-subzone are relatively close to the contact zone between the Mt. Kunlun and the Tarim terrane. The space-time distribution, petrological and geochemical features can be explained by a model of southward intraplate subduction of the Tarim terrane.Keywords
This publication has 5 references indexed in Scilit:
- Geologic Evolution of Northern Tibet: Results of an Expedition to Ulugh MuztaghScience, 1987
- Geomorphic evidence for active faulting in the Altyn Tagh and northern Tibet and qualitative estimates of its contribution to the convergence of India and EurasiaGeology, 1987
- Intracontinental subduction, crust-mantle décollement and crustal-stacking wedge in the Himalayas and other collision beltsGeological Society, London, Special Publications, 1986
- Thin-skinned plate tectonics during Neo-Alpine orogenesisAmerican Journal of Science, 1979
- Geochemistry of eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern TurkeyBeiträge zur Mineralogie und Petrographie, 1976