Construction of Late Devonian Dundunshan arc in the Beishan orogen and its implication for tectonics of southern Central Asian Orogenic Belt

doi:10.1016/j.lithos.2013.11.007

	Construction of Late Devonian Dundunshan arc in the Beishan orogen and its implication for tectonics of southern Central Asian Orogenic Belt
	Guo, Qianqian 1,2; Xiao, Wenjiao 2,3; Hou, Quanlin 1; Windley, Brian F.4; Han, Chunming 3; Tian, Zhonghua 1,3; Song, Dongfang 3
刊名	LITHOS
	2014
卷号	184 页码:361-378
关键词	Beishan Dundunshan arc Devonian Subduction zone retreat Pa leo-Asian Ocean
ISSN号	0024-4937
DOI	10.1016/j.lithos.2013.11.007
文献子类	Article
英文摘要	The Beishan orogen, located in the southern Central Asian Orogenic Belt, was formed by subduction-accretionary processes in the Paleozoic, and so provides key constraints on the current international controversy regarding the duration of the orogenesis and the time of its termination and formation of the final suture. This paper concerns the tectonic setting, in the Beishan, of Devonian volcanic and sedimentary rocks that belong to the Dundunshan subduction-generated volcanic arc. The Dundunshan arc comprises metaluminous to weakly peraluminous, calcalkaline andesites, dacites, rhyolites, porphyries and tuffs, which have Late Devonian U-Pb zircon ages of 368.8 +/- 3.1 Ma and 370.9 +/- 13 Ma. The rhyolites have an arc geochemical signature. The Dundunshan sediments are predominantly clastic sandstones, the trace element geochemical data of which indicate derivation from a rhyolitic source with variable degrees of weathering, suggesting an active tectonic provenance. The Dundunshan arc is situated on the southern side of the Huaniushan arc, which, according to current published data, was generated by northward subduction in the Early Paleozoic, and this was followed by the Dundunshan arc in the Late Devonian. It is likely that the northward-dipping subduction zone retreated southwards, giving rise to southward younging of the arcs. Our data provide important constraints on a better understanding of the growth of arcs that dominate the Altaid accretionary orogen. (C) 2013 Elsevier B.V. All rights reserved.
WOS关键词	ZIRCON U-PB ; NW CHINA IMPLICATIONS ; CONTINENTAL-CRUST ; NORTHWEST CHINA ; GEOCHEMICAL CLASSIFICATION ; ACCRETIONARY TECTONICS ; QINLING OROGEN ; ISLAND ARCS ; NE JAPAN ; ICP-MS
WOS研究方向	Geochemistry & Geophysics ; Mineralogy
语种	英语
出版者	ELSEVIER SCIENCE BV
WOS记录号	WOS:000330815000021
资助机构	Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 41302177 ; 41302177 ; 41302177 ; 41302177 ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41190072 ; 41190072 ; 41190072 ; 41190072 ; 41190070 ; 41190070 ; 41190070 ; 41190070 ; 41190071 ; 41190071 ; 41190071 ; 41190071 ; 41202150 ; 41202150 ; 41202150 ; 41202150 ; 40523003) ; 40523003) ; 40523003) ; 40523003) ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 41302177 ; 41302177 ; 41302177 ; 41302177 ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41190072 ; 41190072 ; 41190072 ; 41190072 ; 41190070 ; 41190070 ; 41190070 ; 41190070 ; 41190071 ; 41190071 ; 41190071 ; 41190071 ; 41202150 ; 41202150 ; 41202150 ; 41202150 ; 40523003) ; 40523003) ; 40523003) ; 40523003) ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 41302177 ; 41302177 ; 41302177 ; 41302177 ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41190072 ; 41190072 ; 41190072 ; 41190072 ; 41190070 ; 41190070 ; 41190070 ; 41190070 ; 41190071 ; 41190071 ; 41190071 ; 41190071 ; 41202150 ; 41202150 ; 41202150 ; 41202150 ; 40523003) ; 40523003) ; 40523003) ; 40523003) ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Bureau of Science and Technology for Resource and Environment, Chinese National Basic Research 973 Program(2014CB440801 ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Innovative Program of the Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; One Hundred Talent Program B of the Chinese Academy of Sciences ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; National Natural Science Foundation of China(41230207 ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 2007CB411307) ; 41302177 ; 41302177 ; 41302177 ; 41302177 ; 41390441 ; 41390441 ; 41390441 ; 41390441 ; 41190072 ; 41190072 ; 41190072 ; 41190072 ; 41190070 ; 41190070 ; 41190070 ; 41190070 ; 41190071 ; 41190071 ; 41190071 ; 41190071 ; 41202150 ; 41202150 ; 41202150 ; 41202150 ; 40523003) ; 40523003) ; 40523003) ; 40523003)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/84804]
专题	中国科学院地质与地球物理研究所
通讯作者	Xiao, Wenjiao
作者单位	1.Univ Chinese Acad Sci, Key Lab Computat Geodynam, Beijing 100049, Peoples R China 2.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Xinjiang Res Ctr Mineral Resources, Urumqi 830011, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 4.Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England
推荐引用方式 GB/T 7714	Guo, Qianqian,Xiao, Wenjiao,Hou, Quanlin,et al. Construction of Late Devonian Dundunshan arc in the Beishan orogen and its implication for tectonics of southern Central Asian Orogenic Belt[J]. LITHOS,2014,184:361-378.
APA	Guo, Qianqian.,Xiao, Wenjiao.,Hou, Quanlin.,Windley, Brian F..,Han, Chunming.,...&Song, Dongfang.(2014).Construction of Late Devonian Dundunshan arc in the Beishan orogen and its implication for tectonics of southern Central Asian Orogenic Belt.LITHOS,184,361-378.
MLA	Guo, Qianqian,et al."Construction of Late Devonian Dundunshan arc in the Beishan orogen and its implication for tectonics of southern Central Asian Orogenic Belt".LITHOS 184(2014):361-378.