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黔西南"水银洞式"金矿成因研究
引用本文:唐波,张敏,黄建国,张竹如,聂爱国.黔西南"水银洞式"金矿成因研究[J].矿物学报,2007,27(3):450-455.
作者姓名:唐波  张敏  黄建国  张竹如  聂爱国
作者单位:贵州大学,资源与环境工程学院,贵州,贵阳,550003
基金项目:贵州省高层次人才科研条件特助经费项目(TZJF2006-5号);贵州大学矿物学岩石学矿床学博士点专题建设项目(2006)
摘    要:水银洞式金矿受控于上二叠统龙潭组,其沉积环境为同生断裂夹持的泻湖.潮坪.局限台地。矿石宏观及显微组构表现为沉积-成岩特征,硫同位素、稀土元素、金及微量元素组合反映矿石与围岩特征一致,沉积-成岩期是水银洞式金矿主成矿期。

关 键 词:水银洞式金矿  矿石显微组构  微量元素  沉积环境  沉积-成岩成因
文章编号:1000-4734(2007)03-0450-06
收稿时间:2007-05-15
修稿时间:2007年5月15日

RESEARCH ON THE GENESIS OF THE SHUIYINDONG GOLD DEPOSIT
TANG Bo, ZHANG Min, HUANG Jjian-guo, ZHANG Zhu-ru.RESEARCH ON THE GENESIS OF THE SHUIYINDONG GOLD DEPOSIT[J].Acta Mineralogica Sinica,2007,27(3):450-455.
Authors:TANG Bo  ZHANG Min  HUANG Jjian-guo  ZHANG Zhu-ru
Abstract:The Shuiyindong gold deposit was hosted in the strata of the Permian Longtan Formation, the depositional environment of the Shuiyindong deposit is alagoon-tide fiat-limited mesa which was retained by contemporaneous faults. The macroscopical characteristics and micrographic fabrics of ores manifest the sedimentation diagenesis characteristics. Sulfur isotopes, rare-earth elements, gold and trace element association reflected that the ores and wall rocks have the same characteristics. The period of sedimentation diagenesisis the main metallogenic period of the Shuiyindong gold deposit.
Keywords:Shuiyindong gold deposit  ore micrographic fabric  trace element  depositional environment  sedimentation diageno-genesis
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