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贵州省三都-丹寨成矿带中卡林型金矿地球化学特征及成矿物质来源初探
谢卓君; 夏勇; 闫宝文; 王泽鹏; 谭亲平; 伍守荣; 范二川
2014
Source Publication矿物岩石地球化学通报
Issue3Pages:326-333
Abstract为探讨三都-丹寨成矿带中卡林型金矿地球化学特征及成矿物质来源,总结了最近的研究成果以及相关数据,结果表明,三都-丹寨卡林型金矿中与成矿相关的方解石、萤石呈现中稀土富集型,方解石δ13 CPDB=-1.61~-5.82‰,δ18 OSMOW=13.97~19.24‰,辉锑矿和雄黄δ34S=14.5‰~22.37‰,辉锑矿和辰砂208Pb/204Pb=37.160~40.330,207 Pb/204 Pb=15.351~16.330,206Pb/204Pb=17.101~20.080,表明三都-丹寨卡林型金矿成矿物质(碳、氧、硫、铅)可能主要来自该区地层,与黔西南卡林型金矿(成矿物质可能主要来自深部岩浆)有明显区别。其δD和δ18 O值显示成矿流体可能主要为卤水和变质流体组成的混合流体,并且到达浅部时混入了大气降水,成矿流体在其演化过程中,可能与有机质发生了同位素交换,或者发生过多期成矿作用。
Keyword卡林型金矿 地球化学特征 卡林型金矿对比 排庭金矿床 苗龙金矿床
Subject Area矿床地球化学
Indexed ByCSCD
Language中文
CSCD IDCSCD:5182489
Citation statistics
Cited Times:4[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/6707
Collection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
Recommended Citation
GB/T 7714
谢卓君,夏勇,闫宝文,等. 贵州省三都-丹寨成矿带中卡林型金矿地球化学特征及成矿物质来源初探[J]. 矿物岩石地球化学通报,2014(3):326-333.
APA 谢卓君.,夏勇.,闫宝文.,王泽鹏.,谭亲平.,...&范二川.(2014).贵州省三都-丹寨成矿带中卡林型金矿地球化学特征及成矿物质来源初探.矿物岩石地球化学通报(3),326-333.
MLA 谢卓君,et al."贵州省三都-丹寨成矿带中卡林型金矿地球化学特征及成矿物质来源初探".矿物岩石地球化学通报 .3(2014):326-333.
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