| 金龙山-丘岭卡林型金矿床成矿特征 |
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| 引用本文： | 张复新,马建秦.金龙山-丘岭卡林型金矿床成矿特征[J].地质与勘探,1999,35(5):20-23. |
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| 作者姓名： | 张复新 马建秦 |
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| 作者单位： | 1. 西北大学地质系·西安·710069
2. 中国科学院贵阳地球化学研究所·贵阳·550002 |
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| 摘 要： | 金龙山—丘岭卡林型金矿床产于华北与扬子两地块会聚结合带的扩张海盆复杂岩相古地理沉积环境中。通过海底火山热液作用和生物活动的沉积成矿作用，形成成矿元素初始富集的矿源层。经后期叠加改造地质作用形成工业矿体
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| 关 键 词： | 卡林型金矿 成矿作用 金龙山-丘岭 秦岭 |
| 修稿时间： | 1997-10-00 |
METALLOGENIC CHARACTERISTICS OF THE JINLONGSHAN-QIULING CARLIN TYPE GOLD DEPOSIT |
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| Zhang Fuxin,Ma Jianqin.METALLOGENIC CHARACTERISTICS OF THE JINLONGSHAN-QIULING CARLIN TYPE GOLD DEPOSIT[J].Geology and Prospecting,1999,35(5):20-23. |
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| Authors: | Zhang Fuxin Ma Jianqin |
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| Abstract: | The Jinlongshan-Qiuling carlin type gold deposit was formed under paleosedimentary environments with complicated lithofacies and in the spreading marine basin on the convergence between north China platform and Yangtze platform. The evolution of the deposit witnessed the formation of source bed with preliminary enrichment of ore-forming elements by marine volcanism and organism, and then mineralization by reformation. |
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| Keywords: | carlin gold deposit mineralization Jinlongshan-Qiuling Qinling |
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