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	Crustal Melting and Flow beneath Northern Tibet: Evidence from Mid-Miocene to Quaternary Strongly Peraluminous Rhyolites in the Southern Kunlun Range
	Wang, Qiang[1,2,3]; Chung, Sun-Lin[4]; Li, Xian-Hua[5]; Wyman, Derek[6]; Li, Zheng-Xiang[2,3]; Sun, Wei-Dong[1]; Qiu, Hua-Ning[1]; Liu, Yong-Sheng[7]; Zhu, Ying-Tang[8]
刊名	JOURNAL OF PETROLOGY
	2012
卷号	53页码:2523-2566
关键词	Tibet crustal melting crustal flow low-velocity zone crustal thickening plateau growth
URL标识	查看原文
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/2246569
专题	华南理工大学
作者单位	1.[1]Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Guangdong, Peoples R China 2.[2]Curtin Univ Technol, ARC Ctr Excellence Core Crust Fluid Syst CCFS, Perth, WA 6845, Australia 3.[3]Curtin Univ Technol, Inst Geosci Res TIGER, Dept Appl Geol, Perth, WA 6845, Australia 4.[4]Natl Taiwan Univ, Dept Geosci, Taipei 10617, Taiwan 5.[5]Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 6.[6]Univ Sydney, Sch Geosci, Sydney, NSW 2006, Australia 7.[7]China Univ Geosci, Fac Earth Sci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China 8.[8]Chengdu Univ Technol, Sedimentary Geol Inst, Chengdu 610059, Peoples R China
推荐引用方式 GB/T 7714	Wang, Qiang[1,2,3],Chung, Sun-Lin[4],Li, Xian-Hua[5],et al. Crustal Melting and Flow beneath Northern Tibet: Evidence from Mid-Miocene to Quaternary Strongly Peraluminous Rhyolites in the Southern Kunlun Range[J]. JOURNAL OF PETROLOGY,2012,53:2523-2566.
APA	Wang, Qiang[1,2,3].,Chung, Sun-Lin[4].,Li, Xian-Hua[5].,Wyman, Derek[6].,Li, Zheng-Xiang[2,3].,...&Zhu, Ying-Tang[8].(2012).Crustal Melting and Flow beneath Northern Tibet: Evidence from Mid-Miocene to Quaternary Strongly Peraluminous Rhyolites in the Southern Kunlun Range.JOURNAL OF PETROLOGY,53,2523-2566.
MLA	Wang, Qiang[1,2,3],et al."Crustal Melting and Flow beneath Northern Tibet: Evidence from Mid-Miocene to Quaternary Strongly Peraluminous Rhyolites in the Southern Kunlun Range".JOURNAL OF PETROLOGY 53(2012):2523-2566.

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