Geochronology and petrogenesis of granitoids and associated mafic   enclaves from Xiate in Chinese Southwest Tianshan: Implications for   early Paleozoic tectonic evolution

doi:10.1016/j.jseaes.2015.09.024

CORC > 北京大学 > 地球与空间科学学院

	Geochronology and petrogenesis of granitoids and associated mafic enclaves from Xiate in Chinese Southwest Tianshan: Implications for early Paleozoic tectonic evolution
	Gou, Long-Long ; Zhang, Li-Fei
刊名	JOURNAL OF ASIAN EARTH SCIENCES
	2016
关键词	Granitoids Continent marginal arc Southwest Tianshan Magma mixing Central Asian Orogenic Belt ZIRCON U-PB ASIAN OROGENIC BELT KYRGYZ TIEN-SHAN ULTRAHIGH-PRESSURE METAMORPHISM PHANEROZOIC CRUSTAL GROWTH UNDERPLATED BASALTIC CRUST S-TYPE GRANITES NW CHINA WESTERN TIANSHAN CONTINENTAL GROWTH
DOI	10.1016/j.jseaes.2015.09.024
英文摘要	Mineral compositions, in-situ zircon U-Pb and Hf isotopes, and whole-rock major-trace elements and Sr-Nd isotopes are reported for the host granitoids and associated mafic microgranular enclaves (MMEs) in Dongdeguli valley, and the Changawuzi mylonitic pluton, in the Southwest Tianshan, NW China. The Dongdeguli host granitoids have LA-ICP-MS zircon U-Pb ages of 446 +/- 2 Ma and 443 +/- 3 Ma, which are comparable with those (436 +/- 6 Ma and 446 +/- 23 Ma) of their enclaves. Both the host granitoids and MMEs have relatively high initial Sr-87/Sr-86 ratios and negative epsilon(Nd)(t) values. The MMEs are enriched in large ion lithophile and light rare earth elements but depleted in high field strength elements, and they are interpreted as melts derived from the fluids/melts metasomatized mantle wedge. The emplacement of mafic arc magma is inferred to cause the partial melting of ancient crust of Yili-Central Tianshan Block, which formed the granitic magma. Magma mixing model is proposed for the origin of the host granitoids and their mafic enclaves in the Dongdeguli valley. The Changawuzi mylonitic pluton has a SHRIMP zircon U-Pb age of 453 +/- 4 Ma. It has relatively low SiO2 content, high MgO content, and negative whole-rock epsilon(Nd)(t) values and zircon epsilon(Hf)(t) values, with two-stage Nd model ages of 1.67-1.7 Ga and two-stage Hf model ages of 1635-1760 Ma, respectively. These results indicate that the Changawuzi mylonitic pluton was derived from partial melting of Paleoproterozoic crustal rocks, with involvement of some mantle-derived magma. The Dongdeguli granitoids,and associated MMEs, and the Changawuzi mylonitic pluton, were formed by the northward subduction of paleo-South Tianshan oceanic crust in the Late Ordovician-Early Silurian period. (c) 2015 Elsevier Ltd. All rights reserved.; National Natural Science Foundation of China [41330210, 41302036, 41272069]; Foundation of State Key Laboratory of Continental Dynamics [BJ08133-12]; Natural Science Foundation of Northwest University, China [12NW29]; Start-up Research Foundation of Northwest University, China [PR12104]; SCI(E); ARTICLE; LLgou@nwu.edu.cn; 40-61; 115
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/438991]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	Gou, Long-Long,Zhang, Li-Fei. Geochronology and petrogenesis of granitoids and associated mafic enclaves from Xiate in Chinese Southwest Tianshan: Implications for early Paleozoic tectonic evolution[J]. JOURNAL OF ASIAN EARTH SCIENCES,2016.
APA	Gou, Long-Long,&Zhang, Li-Fei.(2016).Geochronology and petrogenesis of granitoids and associated mafic enclaves from Xiate in Chinese Southwest Tianshan: Implications for early Paleozoic tectonic evolution.JOURNAL OF ASIAN EARTH SCIENCES.
MLA	Gou, Long-Long,et al."Geochronology and petrogenesis of granitoids and associated mafic enclaves from Xiate in Chinese Southwest Tianshan: Implications for early Paleozoic tectonic evolution".JOURNAL OF ASIAN EARTH SCIENCES (2016).