| 驼背山锑矿床地质特征及成矿机理浅析 |
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| 引用本文： | 高奉林,叶少贞.驼背山锑矿床地质特征及成矿机理浅析[J].化工矿产地质,2006,28(3):133-139. |
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| 作者姓名： | 高奉林 叶少贞 |
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| 作者单位： | 江西省地质矿产勘查开发局赣西北大队,江西,九江,332000 |
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| 摘 要： | 驼背山锑矿床赋存于武宁-新柘林复式向斜南翼之次级驼背山背斜的西端轴部及北翼,矿床受构造、岩性、岩浆岩、水文等综合条件控制。矿体呈层状、似层状、扁豆状产于沿次级背斜轴部及附近两翼展布的层间硅化破碎带内。通过对成矿物质来源、水源及热源,成矿地质、成矿物理、化学等进行分析、推断,其形成经历了多期次、多阶段的构造运动和地热事件,在一定的构造、岩浆岩、岩性、地热、水文等地质条件和一定物理、化学条件下形成的。该矿床类型为地热流体型锑矿床。
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| 关 键 词： | 地质特征 成矿机理 地热流体 锑矿 驼背山 |
| 文章编号： | 1006-5296(2006)03-0133-07 |
| 收稿时间： | 2006-03-27 |
| 修稿时间： | 2006-07-26 |
SIMPLE ANALYSIS OF THE GEOLOGIC FEATURE AND THE METALLOGENIC MECHANISMOF THE TUOBEISHAN STIBIUM |
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| Gao Fenglin,Ye Shaozhen.SIMPLE ANALYSIS OF THE GEOLOGIC FEATURE AND THE METALLOGENIC MECHANISMOF THE TUOBEISHAN STIBIUM[J].Geology of Chemical Minerals,2006,28(3):133-139. |
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| Authors: | Gao Fenglin Ye Shaozhen |
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| Institution: | Geological Party of Jiangxi Northwest, Jiangxi Geological Mineral Prospecting and Exploiting Bureau, Jiujiang, Jiangxi, 332000, China |
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| Abstract: | The Tuobeishan stibium deposited in west axial region and north side of the Tuobeishan anticline,which is the secondary anticline of Wuning-Xintuolin synclinorium. The ore was controlled by structure,lithology, magmatite,and hydrology,etc. The ore developed in the siliconizing interlayer fracture zone, spreading around the secondary anticlinal axis and its sides, occurrences in layers,bedlike and phacoidal. Analyzing the metallogenic mineral source, water source,heat source,geology, physics,chemistry,it can be inferred that in the course there are multistage tectogenesis and geothermal events,and the ore is a geothermal fluidal stibium forming in the certain geologic conditions-structure, magmatite,lithology,geotherm,and hydrology-and physical-chemical conditions. |
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| Keywords: | geologic feature metallogenic mechanism geothermal fluid stibium Tuobeishan |
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