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| 新疆彩霞山铅锌矿床成因分析及与MVT型矿床成因对比 | |
| 引用本文： | 彭明兴,桑少杰,朱才,陈杰,吴礼斌,梁婷,吴雪晶,吴慧平.新疆彩霞山铅锌矿床成因分析及与MVT型矿床成因对比[J].新疆地质,2007,25(4):373-378. |
| 作者姓名： | 彭明兴 桑少杰 朱才 陈杰 吴礼斌 梁婷 吴雪晶 吴慧平 |
| 作者单位： | 1. 新疆维吾尔自治区地质矿产勘查开发局第一地质大队,新疆,昌吉,831100 2. 云南省岩土工程勘察设计研究院,曲靖分院,云南,曲靖,655000 3. 长安大学地球科学与国土资源学院,陕西,西安,710054 |
| 基金项目： | 新疆维吾尔自治区地质矿产勘查开发局地质勘查项目 |
| 摘 要： | 彩霞山铅锌矿床位于塔里木板块北缘活动带卡瓦布拉克-星星峡中间地块,容矿地层为长城系星星峡群,含矿岩性为角砾状硅化粉砂岩、白云石大理岩.通过对矿体特征、稳定同位素、流体包裹体、微量元素等分析,认为彩霞山铅锌矿床成因类型为碎屑岩-碳酸盐岩容矿的后生层控-热液改造型矿床.通过与我国广东凡口铅锌矿床、新疆卡兰古铅锌矿床成因对比研究发现,彩霞山铅锌矿床与二者成因特征类似,具有MVT型矿床成因特征. |
| 关 键 词： | 新疆 彩霞山 铅锌矿床 成因分析 对比 |
| 文章编号： | 1000-8845(2007)04-373-06 |
| 修稿时间： | 2007年8月9日 |
FORMING ANALYSIS OF THE CAIXIA LEAD-ZINC DEPOSIT XINJIANG AND COMPARSON WITH THE MVT DEPOSIT FORMING |
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| PENG Ming-xing,SANG Shao-jie,ZHU Cai,CHEN Jie,WU Li-bin,LIANG Ting,WU Xue-jing,WU Hui-ping.FORMING ANALYSIS OF THE CAIXIA LEAD-ZINC DEPOSIT XINJIANG AND COMPARSON WITH THE MVT DEPOSIT FORMING[J].Xinjiang Geology,2007,25(4):373-378. | |
| Authors: | PENG Ming-xing SANG Shao-jie ZHU Cai CHEN Jie WU Li-bin LIANG Ting WU Xue-jing WU Hui-ping |
| Abstract: | The Caixia lead-zinc deposit is located in the middle blockof Kawabulake-Xingxingxia at northern active margin of the Talimu plate.The ore-bearing strata are the ChX.The rock of the lead-zinc deposit is mainly siliconed silt in general,others is contained dolomitized marble. Studying on the mine body characteristics,Stable isotope,flow inclusion, trace elemen0]t and so on, the Caixia lead-zinc deposit forming type is epigenesis sedimentation-hydrothermal reconstruction which ored mineral clastic rock and carbonate.Though studying with Fangkou Guangdong and Kalangu lead-zinc deposit of Xinjiang, they have similar forming characteristics of MVT lead-zinc deposit. |
| Keywords: | Xinjiang Caixia Lead-zinc deposit Forming analysis correlate |
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