Review of the stable isotope geochemistry of Mesozoic igneous rocks and Cu-Au deposits along the middle-lower Yangtze Metallogenic Belt, China

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	Review of the stable isotope geochemistry of Mesozoic igneous rocks and Cu-Au deposits along the middle-lower Yangtze Metallogenic Belt, China
	Insung Lee; Xiao-Yong Yang
刊名	International Geology Review
	2011
卷号	53 期号:5-6 页码:741-757
关键词	Porphyry Cu-au Deposits Stable Isotope Geochemistry Sulphur Hydrogen Oxygen Isotopes Middle-lower Yangtze Metallogenic Province
英文摘要	Ore deposition took place in the Yangtze Valley episodically during the Jurassic and Cretaceous periods, generating approximately 200 polymetallic Cu-Fe-Au, Mo, Zn, Pb, and Ag deposits. We analysed the stable isotopes of sulphur, oxygen, and hydrogen from the Cu-Au deposits and correlated our new data with published stable isotope for associated Yanshanian (Mesozoic) igneous rocks. The latter bears a close relationship to Cu-Au mineralization in the area. Cu-Au deposits in the middle-lower Yangtze Valley can be divided into three types: skarn, porphyry, and volcanic. The S-O-H isotopic values allow constraints to be placed on the conditions of origin of these famous Cu-Au ores and their related igneous rocks. Sulphur from the sulphide ores mostly was derived from a magmatic source; however, a few deposits reflect a sedimentary source of sulphur. Oxygen isotope values in quartz from the Shaxi porphyry Cu-Au deposit and from the Tongling skarn Cu-Au deposits range from 2.6 parts per thousand to 12.5 parts per thousand and from -1.3 parts per thousand to 24.5 parts per thousand, respectively; these values represent larger variations compared with those from other Cu-Au deposits in this metallogenic belt. Hydrogen versus oxygen isotope plots of the Cu-Au ore-forming fluids demonstrate that the fluids came from different sources: the most important involved the mixing of magmatic and meteoric water; the second most important was strictly magmatic water; and the third most important may have been a mixture of formation water or meteoric water that had reacted with carbonate wall rocks.
学科主题	矿床地球化学
语种	英语
公开日期	2018-01-05
内容类型	期刊论文
源URL	[http://ir.gyig.ac.cn:8080/handle/352002/7063]
专题	地球化学研究所_矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
推荐引用方式 GB/T 7714	Insung Lee,Xiao-Yong Yang. Review of the stable isotope geochemistry of Mesozoic igneous rocks and Cu-Au deposits along the middle-lower Yangtze Metallogenic Belt, China[J]. International Geology Review,2011,53(5-6):741-757.
APA	Insung Lee,&Xiao-Yong Yang.(2011).Review of the stable isotope geochemistry of Mesozoic igneous rocks and Cu-Au deposits along the middle-lower Yangtze Metallogenic Belt, China.International Geology Review,53(5-6),741-757.
MLA	Insung Lee,et al."Review of the stable isotope geochemistry of Mesozoic igneous rocks and Cu-Au deposits along the middle-lower Yangtze Metallogenic Belt, China".International Geology Review 53.5-6(2011):741-757.