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湘中锡矿山式锑矿成矿物质来源探讨
陶琰; 高振敏; 金景福; 曾令交
2001
Source Publication地质地球化学
Volume29Issue:1Pages:14-20
metadata_24其它
Abstract本文从地屡舍矿性、同岩泉活动的关系厦同住素组成特扯等几十方面进行分析,以阐明湘中鹄矿山式锑矿成矿抽质来源于构造岩策活化作用形成的区域性深郜上升流体。虽煞赋矿层住相对集中,但不存在明显的锑矿源屡。铅同住素矸究表明矿石铅来源于深郜均化紊件下的铅同往素演化系统.与围岩地屡铅同住素明显车同。硫同住素显示矿石硫为均一化程度较高的混合漾源硫。包裹体水氢、氧同住素组成舟于太气降水与初生水之问,为混合水类型。
Keyword湖南
Subject Area中国典型特殊区带大规模成矿作用及其动力学
Funding Organization地矿部定向科研基金(地定96—13)。
Indexed ByCSCD
Language中文
CSCD IDCSCD:576432
Citation statistics
Cited Times:13[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/196
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
陶琰,高振敏,金景福,等. 湘中锡矿山式锑矿成矿物质来源探讨[J]. 地质地球化学,2001,29(1):14-20.
APA 陶琰,高振敏,金景福,&曾令交.(2001).湘中锡矿山式锑矿成矿物质来源探讨.地质地球化学,29(1),14-20.
MLA 陶琰,et al."湘中锡矿山式锑矿成矿物质来源探讨".地质地球化学 29.1(2001):14-20.
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