Genesis of the Jurassic Dongfengbeishan porphyry Mo deposit in Eastern Yanbian, NE China inferred from molybdenite Re-Os and zircon U- Pb ages, and whole-rock elemental and zircon Hf isotopic compositions

doi:10.1016/j.jseaes.2017.12.035

CORC > 地质与地球物理研究所 > 中国科学院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

	Genesis of the Jurassic Dongfengbeishan porphyry Mo deposit in Eastern Yanbian, NE China inferred from molybdenite Re-Os and zircon U- Pb ages, and whole-rock elemental and zircon Hf isotopic compositions
	Guo, Weikang 1,2,3; Zeng, Qingdong 1,2,3; Zhang, Bo 4; Hu, Yanzhong 4
刊名	JOURNAL OF ASIAN EARTH SCIENCES
	2018-10-01
卷号	165 页码:256-269
关键词	Zircon U-Pb Molybdenite Re-Os Geochemistry Hf isotope Dongfengbeishan porphyry Mo deposit
ISSN号	1367-9120
DOI	10.1016/j.jseaes.2017.12.035
英文摘要	The Dongfengbeishan porphyry Mo deposit is located to the southeast of the Lesser Xing'an Range-Zhangguangcai Range metallogenic belt in NE China. LA-ICP-MS zircon U-Pb dating of the Beishan monzogranite yields an age of 194.75 +/- 0.81 Ma. Five molybdenite samples define a Re-Os isochron age of 194.0 +/- 2.0 Ma, suggesting that mineralization was associated with emplacement of the Beishan monzogranitic pluton. Monzogranite samples are classified as high-K calc-alkaline and are relatively enriched in light rare earth elements, depleted in heavy rare earth elements, Nb, Ba, P, Sr, Ti, and Zr, and yield negative Eu anomalies. These characteristics are interpreted to record fractional crystallization of the parental magmas. Zircon (epsilon Hf)(t) values for Beishan monzogranite samples range from + 8.2 to + 15.9, and two-stage model ages (T-DM2) range from 217 to 711 Ma, indicating that the parental magma was produced during partial melting of juvenile lower crust. Combined with previous studies, our data suggest that the Dongfengbeishan porphyry Mo deposit was associated with westward subduction of the paleo-Pacific plate in the Early Jurassic.
资助项目	National Key Research Project of China[2017YFC0601306] ; National Natural Science Foundation of China[41390443] ; National Basic Research Program of China[2013CB429804]
WOS关键词	PLASMA-MASS SPECTROMETRY ; DABIE OROGENIC BELT ; A-TYPE GRANITES ; NORTHEASTERN CHINA ; NORTH CHINA ; HEILONGJIANG PROVINCE ; TECTONIC IMPLICATIONS ; LU-HF ; GEOLOGICAL SIGNIFICANCE ; POLYMETALLIC DEPOSIT
WOS研究方向	Geology
语种	英语
出版者	PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号	WOS:000449447300016
资助机构	National Key Research Project of China ; National Key Research Project of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Key Research Project of China ; National Key Research Project of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Key Research Project of China ; National Key Research Project of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Basic Research Program of China ; National Basic Research Program of China ; National Key Research Project of China ; National Key Research Project of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Basic Research Program of China ; National Basic Research Program of China
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/89428]
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	Zeng, Qingdong
作者单位	1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China 3.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China 4.Hanfeng Min Technol Co Ltd, Jilin 133400, Jilin, Peoples R China
推荐引用方式 GB/T 7714	Guo, Weikang,Zeng, Qingdong,Zhang, Bo,et al. Genesis of the Jurassic Dongfengbeishan porphyry Mo deposit in Eastern Yanbian, NE China inferred from molybdenite Re-Os and zircon U- Pb ages, and whole-rock elemental and zircon Hf isotopic compositions[J]. JOURNAL OF ASIAN EARTH SCIENCES,2018,165:256-269.
APA	Guo, Weikang,Zeng, Qingdong,Zhang, Bo,&Hu, Yanzhong.(2018).Genesis of the Jurassic Dongfengbeishan porphyry Mo deposit in Eastern Yanbian, NE China inferred from molybdenite Re-Os and zircon U- Pb ages, and whole-rock elemental and zircon Hf isotopic compositions.JOURNAL OF ASIAN EARTH SCIENCES,165,256-269.
MLA	Guo, Weikang,et al."Genesis of the Jurassic Dongfengbeishan porphyry Mo deposit in Eastern Yanbian, NE China inferred from molybdenite Re-Os and zircon U- Pb ages, and whole-rock elemental and zircon Hf isotopic compositions".JOURNAL OF ASIAN EARTH SCIENCES 165(2018):256-269.