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Ages and tectonic implications of the mafic-ultramafic-carbonatite intrusive rocks and associated Cu-Ni, Fe-P and apatite-vermiculite deposits from the Quruqtagh district, NW China

文献类型：期刊论文

作者Han, Chunming1,2; Xiao, Wenjiao1,2; Su, Benxun1; Sakyi, Patrick Asamoah3; Ao, Songjian1; Zhang, Jien1; Wan, Bo1,2; Song, Dongfang1; Wang, Zhongmei1
刊名ORE GEOLOGY REVIEWS
出版日期2018-04-01
卷号95页码:1106-1122
关键词SIMS zircon U-Pb Ultramafic-mafic-carbonatite Quruqtagh, Tarim Craton, NW China
ISSN号0169-1368
DOI10.1016/j.oregeorev.2016.07.011
文献子类Article
英文摘要The Tarim Craton is an important tectonic unit and a suitable target to investigate and understand the Proterozoic tectonic framework of the Central Asian Orogenic Belt and supercontinent Rodinia. Precambrian ultramaficmafic-carbonatite rocks are widely distributed in the Quruqtagh domain of NE-Tarim. In the Quruqtagh, Cu-Ni, Fe-P and apatite-vermiculite deposits hosted in the ultramafic-mafic-carbonatite rocks occur in the Xingdi, Qieganbulake, Daxigou, and Kawuliuke. These deposits associated with the ultramafic-mafic-carbonatite rocks in Quruqtagh formed in a period between the Paleoproterozoic and Neoproterozoic. The Paleoproterozoic Fe-P deposit is represented by the Daxigou deposit that yielded a SIMS U-Pb zircon age of 2452 +/- 10 Ma. The other Cu-Ni, Fe-P and apatite-vermiculite deposits, hosted in the ultramafic-mafic rocks, formed in the Neoproterozoic, represented by the Xingdi, Kawuliuke, and Qieganbulake deposits that formed between 812 Ma and 707 Ma. The Paleoproterozoic mineralization event was coincident with the global collisional events that led to the assembly of the Paleo-Mesoproterozoic Columbia (Nuna) supercontinent. And the emplacement of these Neoproterozoic ultramafic-mafic-carbonatite rocks was related to a mantle plume event that led to the breakup of the Tarim Craton from the Rodima supercontinent. (C) 2016 Elsevier B.V. All rights reserved.
WOS关键词NORTHEASTERN TARIM BLOCK ; NORTHWEST CHINA ; ZIRCON GEOCHRONOLOGY ; VOLCANIC-ROCKS ; MANTLE PLUME ; SOUTH CHINA ; RODINIA SUPERCONTINENT ; PRECAMBRIAN EVOLUTION ; LU-HF ; GEOCHEMISTRY
WOS研究方向Geology ; Mineralogy ; Mining & Mineral Processing
语种英语
WOS记录号WOS:000432760500059
出版者ELSEVIER SCIENCE BV
资助机构Summary of the North China block iron ore deposits metallogenic regularity(20,089,950) ; Summary of the North China block iron ore deposits metallogenic regularity(20,089,950) ; Chinese Academy of Sciences(XDB18020203) ; Chinese Academy of Sciences(XDB18020203) ; NSFC(41,230,207 ; NSFC(41,230,207 ; 41,190,075 ; 41,190,075 ; 41,390,441 ; 41,390,441 ; 40,421,303 ; 40,421,303 ; 40,572,043) ; 40,572,043) ; Summary of the North China block iron ore deposits metallogenic regularity(20,089,950) ; Summary of the North China block iron ore deposits metallogenic regularity(20,089,950) ; Chinese Academy of Sciences(XDB18020203) ; Chinese Academy of Sciences(XDB18020203) ; NSFC(41,230,207 ; NSFC(41,230,207 ; 41,190,075 ; 41,190,075 ; 41,390,441 ; 41,390,441 ; 40,421,303 ; 40,421,303 ; 40,572,043) ; 40,572,043) ; Summary of the North China block iron ore deposits metallogenic regularity(20,089,950) ; Summary of the North China block iron ore deposits metallogenic regularity(20,089,950) ; Chinese Academy of Sciences(XDB18020203) ; Chinese Academy of Sciences(XDB18020203) ; NSFC(41,230,207 ; NSFC(41,230,207 ; 41,190,075 ; 41,190,075 ; 41,390,441 ; 41,390,441 ; 40,421,303 ; 40,421,303 ; 40,572,043) ; 40,572,043) ; Summary of the North China block iron ore deposits metallogenic regularity(20,089,950) ; Summary of the North China block iron ore deposits metallogenic regularity(20,089,950) ; Chinese Academy of Sciences(XDB18020203) ; Chinese Academy of Sciences(XDB18020203) ; NSFC(41,230,207 ; NSFC(41,230,207 ; 41,190,075 ; 41,190,075 ; 41,390,441 ; 41,390,441 ; 40,421,303 ; 40,421,303 ; 40,572,043) ; 40,572,043)
源URL[http://ir.iggcas.ac.cn/handle/132A11/88206]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Han, Chunming
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resource, Beijing 100029, Peoples R China
2.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
3.Univ Ghana, Dept Earth Sci, POB LG 58, Legon, Ghana
推荐引用方式
GB/T 7714		 Han, Chunming,Xiao, Wenjiao,Su, Benxun,et al. Ages and tectonic implications of the mafic-ultramafic-carbonatite intrusive rocks and associated Cu-Ni, Fe-P and apatite-vermiculite deposits from the Quruqtagh district, NW China[J]. ORE GEOLOGY REVIEWS,2018,95:1106-1122.
APA Han, Chunming.,Xiao, Wenjiao.,Su, Benxun.,Sakyi, Patrick Asamoah.,Ao, Songjian.,...&Wang, Zhongmei.(2018).Ages and tectonic implications of the mafic-ultramafic-carbonatite intrusive rocks and associated Cu-Ni, Fe-P and apatite-vermiculite deposits from the Quruqtagh district, NW China.ORE GEOLOGY REVIEWS,95,1106-1122.
MLA Han, Chunming,et al."Ages and tectonic implications of the mafic-ultramafic-carbonatite intrusive rocks and associated Cu-Ni, Fe-P and apatite-vermiculite deposits from the Quruqtagh district, NW China".ORE GEOLOGY REVIEWS 95(2018):1106-1122.

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来源：地质与地球物理研究所

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