楚雄盆地砂岩铜矿床同位素特征及矿床成因 |
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引用本文: | 陈根文,吴延之,夏斌,王核,钟志洪,王国强.楚雄盆地砂岩铜矿床同位素特征及矿床成因[J].大地构造与成矿学,2002,26(3):279-284. |
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作者姓名: | 陈根文 吴延之 夏斌 王核 钟志洪 王国强 |
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作者单位: | 1. 中国科学院广州地球化学研究所,广东,广州,510650 2. 中南大学地质研究所,湖南,长沙,410083 |
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基金项目: | 中国科学院知识创新工程项目,国家自然科学基金,KZCX2-SW-117,KZCX2-101-04,40072022,, |
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摘 要: | 楚雄盆地砂岩铜矿形成于白垩系高峰寺组凹地苴段、马头山组六苴段和大村段,以六苴、郝家河及大村铜矿床为代表。不论是硫同位素,还是氢氧同位素、铅同位素,六苴铜矿床和郝家河铜矿床均不相同。六苴铜矿硫化物中的硫以来自围岩为主,成矿溶液来自上部天水和建造水,成矿金属物质来自围岩,推测成岩成矿作用是主要矿化机制。而郝家河铜矿,成矿物质更多的是来自地下深处,与深部地下水循环作用有关,表明郝家河铜矿床以改造成矿为主。
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关 键 词: | 砂岩铜矿 同位素特征 矿床成因 六苴铜矿 郝家河铜矿 楚雄盆地 |
文章编号: | 1001-1552(2002)03-279-06 |
修稿时间: | 2002年1月15日 |
ISOTOPIC CHARACTERISTICS AND GENESIS OF THE SANDSTONE-TYPE COPPER DEPOSITS IN THE CHUXIONG BASIN, YUNNAN PROVINCE |
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Abstract: | The sandstone-type Cu deposits in th e Chuxiong basin occur in the Cretaceous Gaofengsi Formation and Maotoushan Formation and these o re deposits are represented by the Luju copper deposit and Haojiahe copper deposit.There are difference between the sulfur,hydrogen,oxygen and lead isotope of the Luju copper deposit and Haojiahe copper d eposit.The sulfur of the Luju copper deposit came from the host,the mineralized solution from the rain a nd formation water,and the copper mi ght stem from the country rocks.It shows that minerogenesis may be main ly formed by diagenesis.In the Haoji ahe copper deposit,mineralized material came from deep-seated sour ce,and the minerogenesis is connected with the deep-water current. |
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Keywords: | Chuxiong basin standstone-type co pper deposit isotopic characteris tics ore genesis Luju copper deposit Haojiahe copper dep osit |
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