| 贵州松桃地区早震旦世大塘坡期沉积环境及锰矿成因 |
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| 引用本文： | 夏文杰,雷建喜. 贵州松桃地区早震旦世大塘坡期沉积环境及锰矿成因[J]. 成都理工大学学报(自然科学版), 1989, 0(1) |
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| 作者姓名： | 夏文杰 雷建喜 |
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| 作者单位： | 成都地质学院(夏文杰)，中国地质大学(雷建喜) |
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| 摘 要： | ![]()
该区大塘坡期为泻湖-潮坪环境,对锰矿床的形成具有明显的控制作用。作者还以矿床地质特征为依据,结合化学成分测定、同位素资料、稀土元素分析、阴极发光技术和数理统计分析,提出该矿床锰质来源于海底火山喷发的观点。
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| 关 键 词： | 泻湖-潮坪 锰矿床 菱锰矿 海底火山喷发 |
SEDIMENTARY ENVIRONMENT OF THE DATANGPO PERIOD, EARLY SINIAN AND GENESIS OF THE MANGANESE ORES IN SONGTAO DISTRICT, GUIZHOU PROVINCE |
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| Xia Wenjie,Lei Jianxi Chengdu College of Geology China University of Geosciences,Wuhan. SEDIMENTARY ENVIRONMENT OF THE DATANGPO PERIOD, EARLY SINIAN AND GENESIS OF THE MANGANESE ORES IN SONGTAO DISTRICT, GUIZHOU PROVINCE[J]. Journal of Chengdu University of Technology: Sci & Technol Ed, 1989, 0(1) |
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| Authors: | Xia Wenjie Lei Jianxi Chengdu College of Geology China University of Geosciences Wuhan |
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| Abstract: | ![]()
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| Keywords: | lagoon-tidal flat manganese deposit rhodochrosite submarine volcanic eruption |
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