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浅论扬子西南缘卡林型金矿成矿物质来源及有机质在成矿过程中的作用
任涛; 张兴春; 王守旭; 冷成彪
Corresponding Author张兴春
2008
Source Publication地质找矿论丛
Volume23Issue:4Pages:287-291,319
metadata_24其它
Abstract在前人研究的基础上,对扬子西缘卡林型金矿采用稳定同位素和生物化学试验方法,分析赋金地层中有机质的种类、性质和有机质与金矿的关系,讨论有机质在金元素富集、迁移、成矿过程中的作用。认为赋金地层与后期岩浆热液发生广泛的交换作用,萃取出成矿物质形成成矿流体,这种富含成矿物质的热液流体在一定的条件下富集成矿。
Keyword卡林型金矿
Subject Area中国典型特殊区带大规模成矿作用及其动力学
Indexed ByCSCD
Language中文
CSCD IDCSCD:3446629
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Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/307
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
Corresponding Author张兴春
Recommended Citation
GB/T 7714
任涛,张兴春,王守旭,等. 浅论扬子西南缘卡林型金矿成矿物质来源及有机质在成矿过程中的作用[J]. 地质找矿论丛,2008,23(4):287-291,319.
APA 任涛,张兴春,王守旭,&冷成彪.(2008).浅论扬子西南缘卡林型金矿成矿物质来源及有机质在成矿过程中的作用.地质找矿论丛,23(4),287-291,319.
MLA 任涛,et al."浅论扬子西南缘卡林型金矿成矿物质来源及有机质在成矿过程中的作用".地质找矿论丛 23.4(2008):287-291,319.
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