Paleozoic subduction-related magmatism in the Duobagou area, Dunhuang block: Constrained by zircon U-Pb geochronology and Lu-Hf isotopes and whole-rock geochemistry of metaigneous rocks

doi:10.1130/L688.1

	Paleozoic subduction-related magmatism in the Duobagou area, Dunhuang block: Constrained by zircon U-Pb geochronology and Lu-Hf isotopes and whole-rock geochemistry of metaigneous rocks
	Wang, Zhong-Mei 1; Han, Chun-Ming 2,3,4; Xiao, Wen-Jiao 1,3,4; Sakyi, Patrick Asamoah 5
刊名	LITHOSPHERE
	2017-12-01
卷号	9 期号:6 页码:1012-1032
ISSN号	1941-8264
DOI	10.1130/L688.1
文献子类	Article
英文摘要	The Dunhuang block, situated at the junction of the Tethyan domain, Tarim craton, North China craton and the Central Asian Orogenic Belt (CAOB), consists mainly of Archean-early Mesoproterozoic basement rocks and Paleozoic metamorphic and magmatic rocks. In this study we performed systematic analyses on the Duobagou metaigneous rocks, including zircon U-Pb ages and Hf isotopes and whole-rock geo-chemistry, to discuss the evolutionary history of the Dunhuang block and the surrounding continental fragments during the Paleozoic.
WOS关键词	ASIAN OROGENIC BELT ; NORTHEASTERN TARIM CRATON ; NW CHINA IMPLICATIONS ; TECTONIC IMPLICATIONS ; METAMORPHIC EVOLUTION ; NORTHWESTERN CHINA ; SOUTHERN ALTAIDS ; VOLCANIC-ROCKS ; GRANITIC-ROCKS ; CONTINENTAL GROWTH
WOS研究方向	Geochemistry & Geophysics ; Geology
语种	英语
出版者	GEOLOGICAL SOC AMER, INC
WOS记录号	WOS:000417374300010
资助机构	National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; 41230207 ; 41230207 ; 41230207 ; 41230207 ; 41202150 ; 41202150 ; 41202150 ; 41202150 ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41102132 ; 41102132 ; 41102132 ; 41102132 ; 41302167) ; 41302167) ; 41302167) ; 41302167) ; National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; 41230207 ; 41230207 ; 41230207 ; 41230207 ; 41202150 ; 41202150 ; 41202150 ; 41202150 ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41102132 ; 41102132 ; 41102132 ; 41102132 ; 41302167) ; 41302167) ; 41302167) ; 41302167) ; National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; 41230207 ; 41230207 ; 41230207 ; 41230207 ; 41202150 ; 41202150 ; 41202150 ; 41202150 ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41102132 ; 41102132 ; 41102132 ; 41102132 ; 41302167) ; 41302167) ; 41302167) ; 41302167) ; National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; National Key Research and Development Program of China(2017YFC0601205) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; 973 Program(2014CB440801) ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National Natural Science Foundation(41272107 ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; National 305 Projects(2011BAB06B04-1) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; China Postdoctoral Foundation(2015M580133) ; 41230207 ; 41230207 ; 41230207 ; 41230207 ; 41202150 ; 41202150 ; 41202150 ; 41202150 ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41102132 ; 41102132 ; 41102132 ; 41102132 ; 41302167) ; 41302167) ; 41302167) ; 41302167)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/82278]
专题	中国科学院地质与地球物理研究所
通讯作者	Wang, Zhong-Mei
作者单位	1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, 19 Beitucheng West Rd, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, 19 Beitucheng West Rd, Beijing 100029, Peoples R China 3.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, 16 Lincui Rd, Beijing 100101, Peoples R China 4.Chinese Acad Sci, Xinjiang Res Ctr Mineral Resources, 818 South Beijing Rd, Urumqi 830011, Xinjiang, Peoples R China 5.Univ Ghana, Sch Phys & Math Sci, Dept Earth Sci, POB LG 58, Legon, Ghana
推荐引用方式 GB/T 7714	Wang, Zhong-Mei,Han, Chun-Ming,Xiao, Wen-Jiao,et al. Paleozoic subduction-related magmatism in the Duobagou area, Dunhuang block: Constrained by zircon U-Pb geochronology and Lu-Hf isotopes and whole-rock geochemistry of metaigneous rocks[J]. LITHOSPHERE,2017,9(6):1012-1032.
APA	Wang, Zhong-Mei,Han, Chun-Ming,Xiao, Wen-Jiao,&Sakyi, Patrick Asamoah.(2017).Paleozoic subduction-related magmatism in the Duobagou area, Dunhuang block: Constrained by zircon U-Pb geochronology and Lu-Hf isotopes and whole-rock geochemistry of metaigneous rocks.LITHOSPHERE,9(6),1012-1032.
MLA	Wang, Zhong-Mei,et al."Paleozoic subduction-related magmatism in the Duobagou area, Dunhuang block: Constrained by zircon U-Pb geochronology and Lu-Hf isotopes and whole-rock geochemistry of metaigneous rocks".LITHOSPHERE 9.6(2017):1012-1032.