Hydrothermal fluid evolution of the Jintingling gold deposit in the Jiaodong peninsula, China: Constraints from U-Pb age, CL imaging, fluid inclusion and stable isotope

doi:10.1016/j.jseaes.2017.12.033

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

	Hydrothermal fluid evolution of the Jintingling gold deposit in the Jiaodong peninsula, China: Constraints from U-Pb age, CL imaging, fluid inclusion and stable isotope
	Ma, Wei-Dong 1,2; Fan, Hong-Rui 1,2,3; Liu, Xuan 1,2,4; Yang, Kui-Feng 1,2,3; Hu, Fang-Fang 1,2,3; Zhao, Kuidong 5; Cai, Ya-Chun 1; Hu, Huan-Long 1,2
刊名	JOURNAL OF ASIAN EARTH SCIENCES
	2018-07-01
卷号	160 页码:287-303
关键词	Geochronology Magmatic fluid Jintingling gold deposit Jiaodong
ISSN号	1367-9120
DOI	10.1016/j.jseaes.2017.12.033
文献子类	Article
英文摘要	The Jintingling gold deposit, located in the Jiaodong peninsula, north China, contains vein-, dissemination- and stockwork-style ores hosted in the Jurassic Linglong granitic pluton. Hydrothermal activities in this deposit are divided into seven stages, including pre-ore massive K-feldspar alteration, specularite-quartz vein (V1), milky quartz +/- sulfide vein (V2), quartz-pyrite vein (V3), massive quartz-sericite-pyrite alteration and gold mineralization, quartz-polymetallic sulfide vein (V4), and quartz-calcite vein (V5). Rhenium-Osmium dating was conducted on molybdenite from V2, yielding an isochron age of 123.3 +/- 3.6 Ma. LA-ICP-MS zircon U-Pb dating yielded 121.5 +/- 1.5 Ma (1 sigma, MSWD = 0.010) for a pre-ore diorite porphyrite dyke and 117.6 +/- 1.2 Ma (1 sigma, MSWD = 0.018) for a post-ore diorite porphyry dyke, respectively. Thus, gold mineralization occurred at 122-118 Ma.
WOS关键词	PORPHYRY-COPPER-DEPOSIT ; LA-ICP-MS ; ULTRAHIGH-PRESSURE TERRANE ; SULU OROGENIC BELT ; PAPUA-NEW-GUINEA ; RE-OS AGES ; EASTERN CHINA ; MOLYBDENUM DEPOSIT ; OXYGEN-ISOTOPE ; GEOCHEMICAL CONSTRAINTS
WOS研究方向	Geology
语种	英语
出版者	PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号	WOS:000434751500019
资助机构	National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105) ; National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105) ; National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105) ; National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Natural Science Foundation of China(41672094) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105) ; National Key R&D Program of China(2016YFC0600105)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/88200]
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	Fan, Hong-Rui
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.Western Washington Univ, Dept Geol, Bellingham, WA 98225 USA 5.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Hubei, Peoples R China
推荐引用方式 GB/T 7714	Ma, Wei-Dong,Fan, Hong-Rui,Liu, Xuan,et al. Hydrothermal fluid evolution of the Jintingling gold deposit in the Jiaodong peninsula, China: Constraints from U-Pb age, CL imaging, fluid inclusion and stable isotope[J]. JOURNAL OF ASIAN EARTH SCIENCES,2018,160:287-303.
APA	Ma, Wei-Dong.,Fan, Hong-Rui.,Liu, Xuan.,Yang, Kui-Feng.,Hu, Fang-Fang.,...&Hu, Huan-Long.(2018).Hydrothermal fluid evolution of the Jintingling gold deposit in the Jiaodong peninsula, China: Constraints from U-Pb age, CL imaging, fluid inclusion and stable isotope.JOURNAL OF ASIAN EARTH SCIENCES,160,287-303.
MLA	Ma, Wei-Dong,et al."Hydrothermal fluid evolution of the Jintingling gold deposit in the Jiaodong peninsula, China: Constraints from U-Pb age, CL imaging, fluid inclusion and stable isotope".JOURNAL OF ASIAN EARTH SCIENCES 160(2018):287-303.