| 祝寿泉.桃江式碳酸锰矿床成因探讨[J].地质找矿论丛,1992,(3):83-90 |
| 桃江式碳酸锰矿床成因探讨 |
| ON THE GENESIS OF THE TAOJIANG TYPE MANGANESE CARBONATE DEPOSIT |
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| DOI：10.6053/j.issn.1001-1412.1992.3. 008 |
| 中文关键词: 桃江式碳酸锰矿床 成因 |
| 英文关键词: |
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| 中文摘要: |
| 桃江式锰矿分布于湖南中部桃江、益阳、安化、宁乡县境内,含矿层位为中奥陶统磨刀溪组,为低磷优质碳酸锰矿床.典型矿床有桃江响涛源锰矿床.它是一种受江南岛群与湘赣交界的水下隆起控制的非补偿边缘海中沉积的矿床.本文对桃江式锰矿形成的岩相古地理环境、矿床地质特征、地球化学特征及矿床成因作简单探讨. |
| 英文摘要: |
| The Taojiang Type manganese deposit is a major high-grade manganese deposit of marine sedimentary type.Source materials were of the Yangtze River Sea.Based on geology of the manganese deposits,chemical Composition of ores and isotopes the deposit is geneticly related to algal activity. |
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