Felsic Magmatic Evolution and the Role of Post-Collisional Process in Continental Crustal Growth at Convergent Margins: Insights from the Western Part of the Central Qilian Belt, Northwestern China

被引:0
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作者
WANG Chao [1 ]
LI Rong-She [1 ]
SMITHIES R.Hugh [2 ]
LI Meng [3 ]
PENG Yan [3 ]
机构
[1] State Key Laboratory of Continental Dynamics,Department of Geology,Northwest University
[2] Geological Survey of Western Australia
[3] Xi'an Center of Geological Survey,China Geological Survey
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中图分类号
P542 [构造运动];
学科分类号
070904 ;
摘要
1 Introduction Long-lived early Palaeozoic magmatism in the Qilian orogen,of the Northeastern Tibet Plateau,formed an extensive linear belt of plutonic and volcanic rocks as a result of subduction of the Proto-Tethyan Ocean beneath,and subsequent accretion of resulting arc crust onto,the proto-margin of the North China Craton(NCC)(Song et
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页码:92 / 93
页数:2
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