| 西藏尼雄矿田日阿铜矿床矽卡岩矿物学特征及地质意义 |
| Received:January 09, 2012 Revised:April 07, 2012 点此下载全文 |
| 引用本文：YU YuShuai,YANG ZhuSen,LIU YingChao,TIAN ShiHong,ZHAO Can,GAO Yuan,JI XianHua,HU WeiZheng,CAO ShengHua.2012.Mineralogical characteristics of skarn in Ri'a copper deposit of Nixiong orefield, Tibet, and their geological significance[J].Mineral Deposits,31(4):775~790 |
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| Author Name | Affiliation | | YU YuShuai | Wuhan Institute of Geology and Mineral Resources, Wuhan 430205,Hubei,China | | YANG ZhuSen | Institute of Mineral Resources,CAGS, Beijing 100037, China | | LIU YingChao | Institute of Geology, CAGS, Beijing 100037, China | | TIAN ShiHong | Institute of Mineral Resources,CAGS, Beijing 100037, China | | ZHAO Can | Wuhan Institute of Geology and Mineral Resources, Wuhan 430205,Hubei,China | | GAO Yuan | Jiangxi Institute of Geological Survey,Nanchang 330201,Jiangxi, China | | JI XianHua | Institute of Mineral Resources,CAGS, Beijing 100037, China
School of Earth Sciences and Resources,China University of Geosciences,Beijing 10083,China | | HU WeiZheng | Jiangxi Institute of Geological Survey,Nanchang 330201,Jiangxi, China | | CAO ShengHua | Jiangxi Institute of Geological Survey,Nanchang 330201,Jiangxi, China |
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| 基金项目:本文受"十一五"国家科技支撑计划项目(2006BAB01A04);国家重点基础研究发展计划973项目(2011CB403100,2009CB421007)和地质调查计划项目(1212010918014)联合资助 |
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| 中文摘要:尼雄矿田位于冈底斯成矿带西段中部隆格尔-南木林岩浆岩带的北侧。日阿铜矿床位于尼雄矿田的东南端,矿体产于晚白垩世侵入岩与下拉组灰岩接触带的矽卡岩或矽卡岩化大理岩中,主要矽卡岩矿物有石榴子石、透辉石、蛇纹石、金云母、绢云母、硅镁石、阳起石、透闪石、绿帘石、绿泥石等。电子探针分析表明,矿区石榴子石主要为钙铁榴石,次为钙铝榴石;辉石以透辉石为主;金云母明显富镁贫铁,且富含挥发分F;闪石类矿物属钙角闪石系列;绿泥石富镁贫铁。推断成矿流体大致经历了5个演化阶段: ① 干矽卡岩阶段,高温(＞450℃)、低pH值、氧化-弱氧化; ② 湿矽卡岩阶段,温度降低,pH值和氧逸度逐渐升高; ③ 氧化物阶段,温度进一步降低,pH值升高(碱性),氧逸度则呈降低趋势; ④ 石英硫化物阶段,中等温度(200~300℃),高pH值(碱性),低氧逸度; ⑤ 碳酸盐阶段,低温(160~203℃),低pH值,低氧逸度。此外,矿区还存在多金属矿化的可能。 |
| 中文关键词:地球化学 矽卡岩 矿物学 电子探针分析 日阿铜矿床 尼雄矿田 西藏 |
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| Mineralogical characteristics of skarn in Ri'a copper deposit of Nixiong orefield, Tibet, and their geological significance |
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| Abstract:The Nixiong orefield is located in northern Longge'er-Nanmulin magmatic belt along the central part of western Gangdise metallogenic belt. The Ri'a copper deposit is in southeast Nixiong ore field. The ore bodies mainly occur in the skarn and skarnized marble, which lie between the intrusive rock and Xiala Formation. The main skarn minerals are garnet, diopside, serpentine, phlogopite, actinolite, humite, tremolite, epidote, chlorite, sericite and so on. Electron microprobe analyses show that the garnet is composed mainly of grossularite (62.08%) and andradite (35.08%). Almost all the pyroxenes belong to diopside. Phlogopites are rich in iron and poor in magnesium, also with features of high F. The amphiboles show characteristics of calc-amphibole. The chlorites are rich in magnesium and poor in iron. According to the above data, the authors infer that the ore-forming fluid might have experienced the following five evolutionary stages: ① dry skarn stage of high temperature (>450℃), low pH, oxidation-weak oxidation; ② wet skarn stage of lower temperature, with gradual increasing pH value and oxygen fugacity; ③ oxide stage of further reducing temperature, increasing pH value (alkaline) and decreasing oxygen fugacity; ④ quartz sulfide stage with temperature down to 200~300℃, high pH (alkaline), low oxygen fugacity; ⑤ carbonate stage of low temperature (160~203℃), low pH and low oxygen fugacity. In addition, there probably exists more metal mineralization in the Ri'a copper deposit. |
| keywords:geochenmistry skarn mineralogy electron microprobe analysis Ri'a copper deposit Nixiong Orefield Tibet |
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