| 阳春盆地锡山钨锡矿床钾长花岗岩的矿物学特征及地质意义 |
| Received:March 05, 2017 Revised:April 24, 2018 点此下载全文 |
| 引用本文：OUYANG ZhiXia,LIU DongHong,WANG LiMing,LIANG JinLong,Wang RuPeng,WU XiaoDong,YANG ShengHu.2018.Mineral characteristics of alkali feldspar granites from Xishan W-Sn deposit inYangchun basin and their geological significance[J].Mineral Deposits,37(4):867~884 |
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| Author Name | Affiliation | E-mail | | OUYANG ZhiXia | Geological Bureau for Nonferrous Metals of Guangdong Province, Guangzhou 510080, China | | | LIU DongHong | Geological Bureau for Nonferrous Metals of Guangdong Province, Guangzhou 510080, China | | | WANG LiMing | Geological Bureau for Nonferrous Metals of Guangdong Province, Guangzhou 510080, China | | | LIANG JinLong | Chengdu University of Technology, Chengdu 610059, Sichuan, China | richardljl04@aliyun.com | | Wang RuPeng | Geological Bureau for Nonferrous Metals of Guangdong Province, Guangzhou 510080, China | | | WU XiaoDong | Geological Bureau for Nonferrous Metals of Guangdong Province, Guangzhou 510080, China | | | YANG ShengHu | Geological Bureau for Nonferrous Metals of Guangdong Province, Guangzhou 510080, China | |
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| 基金项目:本文为国家自然科学基金项目（编号：41702083）、中国博士后科学基金项目（编号：2018T110125、2017M610105）和中国地质调查局地质调查工作项目（编号：12120114015801、1212011120826）共同资助的成果 |
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| 中文摘要:锡山钨锡多金属矿是粤西阳春盆地内一个中型石英脉型矿床，成矿岩体岩性为钾长花岗岩，主要矿物组成为钾长石、斜长石、石英、黑云母，副矿物包括锆石、磷灰石、金红石、钛铁矿和铌铁矿等。文章利用电子探针技术对主要矿物的矿物学特征进行了研究，结果表明花岗岩中斜长石为钠长石，钾长石为透长石，黑云母属于铁叶云母。黑云母化学成分显示其w（Ti）介于0.19~0.39，具有低的氧逸度（log f（O2） < Ni-NiO），指示其有利于钨锡矿床的形成且仍具有较好的找矿潜力。结合已有的区域地质资料，文章认为锡山钨锡多金属矿床是岩石圈伸展背景下的产物。 |
| 中文关键词:地球化学 钾长花岗岩 矿物学特征 锡山钨锡矿 阳春盆地 云开地区 |
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| Mineral characteristics of alkali feldspar granites from Xishan W-Sn deposit inYangchun basin and their geological significance |
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| Abstract:The Xishan W-Sn polymetallic deposit, located in the Yangchun basin of western Guangdong Province, is a medium-sized quartz vein W-Sn deposit. The deposit is temporally and spatially associated with Xishan alkali feldspar granite, which mainly consists of K-feldspar, plagioclase, biotite and quartz. Accessory minerals include zircon, apatite, rutile, ilmenite and niobite. Systematic petrological and mineralogical investigation indicates that the plagioclase is albite, K-feldspar is mainly orthoclase, and biotite is siderophyllite. The Xishan granite has Ti content of 0.19~0.39 and low oxygen fugacity (log f(O2) < Ni-NiO), which is more conducive to the formation of W-Sn deposits and thus exhibits a higher potential. These results, together with previously presented regional geological relationships, suggest that the formation of the Xishan alkali feldspar granite and other Cretaceous magmatism in the region was related to lithospheric extension. |
| keywords:geochemistry alkali feldspar granite mineral characteristics Xishan W-Sn deposit Yangchun basin Yunkai region |
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