中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
首页 机构 成果 学者
  
  1. CAS IR Grid
  2. 地质与地球物理研究所
  3. 中国科学院地质与地球物理研究所
Skarn-mineralized porphyry adakites in the Harlik arc at Kalatage, E. Tianshan (NW China): Slab melting in the Devonian-early Carboniferous in the southern Central Asian Orogenic Belt

文献类型：期刊论文

作者Mao, Qigui1; Yu, Mingjie1; Xiao, Wenjiao2,3,4; Windley, Brian F.5; Li, Yuechen1; Wei, Xiaofeng1; Zhu, Jiangjian1; Lu, Xiaoqiang1
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2018-03-01
卷号153页码:365-378
关键词Adakites Porphyry Cu(Au) deposits Crustal growth Harlirk-Dananhu arc CAOB
ISSN号1367-9120
DOI10.1016/j.jseaes.2017.03.021
文献子类Article
英文摘要The geodynamic control of mineralization in the accretionary evolution of the Central Asian Orogenic Belt (CAOB) has long been controversial. Here we report new field, geochemical and geochronological data on recently defined porphyry and skarn-type ore deposits (Devonian-Early Carboniferous) in the Kalatage area in the middle of the Harlik-Dananhu arc, Eastern Tianshan, NW China in the southern CAOB, with the aim of better understanding the accretionary tectonics and genesis of porphyry and skam-type mineralization. The Yudai porphyry Cu-(Au) deposits and the Xierqu skarn Cu-Fe-(Au) deposits are closely associated with Middle Devonian adakitic diorite porphyries (382-390 Ma), which are talc-alkaline and characterized by high Na2O/K2O ratios and Sr contents (310-1020 ppm), strong depletion of HREE (e.g., Yb = 0.80-1.44 ppm) and Y (7.68-14.50 ppm), and all enriched in Rb, Sr, Ba, K and depleted in Nb and Ti. They are characterized by distinctive Eu positive anomalies, high Na2O contents and MORE-like Sr and Nd isotope signatures (high epsilon(Nd)(t) = +6.1 to +7.0 and low (Sr-87/Sr-86)(i) = 0.70412-0.70462). These adakites most likely formed by melting of a young/hot subducted oceanic slab, and adakites in general are important carriers of porphyry Cu +/- (Au) deposits. Early Carboniferous adakites in the Tuwu area south of Kalatage are known to have similar features. Therefore, skarn-mineralized porphyry adakites get younger from north to south, suggesting southward migration of the Harlik-Dananhu arc from 390 Ma to 322 Ma. These data indicate that partial melting of hot (and/or young) oceanic crustal slabs were an important mechanism of accretionary crustal growth and mineralization in the southern CAOB.
WOS关键词PHANEROZOIC CRUSTAL GROWTH ; U-PB GEOCHRONOLOGY ; A-TYPE GRANITES ; EASTERN TIANSHAN ; GEOCHEMICAL CONSTRAINTS ; CONTINENTAL GROWTH ; TECTONIC EVOLUTION ; ISOTOPIC EVIDENCE ; ACCRETIONARY OROGENESIS ; PALEOZOIC ACCRETIONARY
WOS研究方向Geology
语种英语
WOS记录号WOS:000424181200020
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 41230207 ; 41230207 ; 41230207 ; 41230207 ; 41190075 ; 41190075 ; 41190075 ; 41190075 ; 41202150) ; 41202150) ; 41202150) ; 41202150) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 41230207 ; 41230207 ; 41230207 ; 41230207 ; 41190075 ; 41190075 ; 41190075 ; 41190075 ; 41202150) ; 41202150) ; 41202150) ; 41202150) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 41230207 ; 41230207 ; 41230207 ; 41230207 ; 41190075 ; 41190075 ; 41190075 ; 41190075 ; 41202150) ; 41202150) ; 41202150) ; 41202150) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Ministry of Land and Resources for the public welfare industry research(201411026-1) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese Geological Survey Project(DD20160071) ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; Chinese State 305 Project(2011BAB06B04-03 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; National Natural Science Foundation of China(41390441 ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; Chinese Academy of Sciences (CAS)(XDB18020203) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; CAS(QYZDJ-SSW-SYS012) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 2011BAB06B04-1) ; 41230207 ; 41230207 ; 41230207 ; 41230207 ; 41190075 ; 41190075 ; 41190075 ; 41190075 ; 41202150) ; 41202150) ; 41202150) ; 41202150)
源URL[http://ir.iggcas.ac.cn/handle/132A11/82844]  
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.Beijing Inst Geol Mineral Resources, Beijing 100012, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China
4.Univ Chinese Acad Sci, Beijing, Peoples R China
5.Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England
推荐引用方式
GB/T 7714		 Mao, Qigui,Yu, Mingjie,Xiao, Wenjiao,et al. Skarn-mineralized porphyry adakites in the Harlik arc at Kalatage, E. Tianshan (NW China): Slab melting in the Devonian-early Carboniferous in the southern Central Asian Orogenic Belt[J]. JOURNAL OF ASIAN EARTH SCIENCES,2018,153:365-378.
APA Mao, Qigui.,Yu, Mingjie.,Xiao, Wenjiao.,Windley, Brian F..,Li, Yuechen.,...&Lu, Xiaoqiang.(2018).Skarn-mineralized porphyry adakites in the Harlik arc at Kalatage, E. Tianshan (NW China): Slab melting in the Devonian-early Carboniferous in the southern Central Asian Orogenic Belt.JOURNAL OF ASIAN EARTH SCIENCES,153,365-378.
MLA Mao, Qigui,et al."Skarn-mineralized porphyry adakites in the Harlik arc at Kalatage, E. Tianshan (NW China): Slab melting in the Devonian-early Carboniferous in the southern Central Asian Orogenic Belt".JOURNAL OF ASIAN EARTH SCIENCES 153(2018):365-378.

入库方式： OAI收割

来源：地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。