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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
|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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D O I:
暂无
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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