| 贺兰山北段葫鲁斯太煤矿区山西组中、下部沉积相与沉积模式 |
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| 引用本文： | 钟蓉,陈钟惠,傅泽明,杨年厚.贺兰山北段葫鲁斯太煤矿区山西组中、下部沉积相与沉积模式[J].地球学报,1981,3(1):31-45. |
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| 作者姓名： | 钟蓉 陈钟惠 傅泽明 杨年厚 |
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| 作者单位： | 中国地质科学院地质力学研究所;武汉地质学院;武汉地质学院;内蒙古自治区煤田地质勘探公司 |
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| 摘 要： | <正> 葫鲁斯太矿区其大地构造位置处于祁、吕、贺山字型脊柱之北段。矿区内自中石炭世到晚二叠世的晚古生代地层发育齐全,出露良好。本溪群不整合于寒武系之上,其上地层均为连续沉积。全区基本上为一缓倾斜的单斜构造,走向北西20—30度,倾向南西,倾角20—30度,属葫鲁斯大大向斜之东翼。除矿区南端外,本区构造都比较简单。
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NOTE ON SEDIMENTARY FACIES AND SEDIMENTARY MODELS OF THE MIDDLE AND LOWER SHANXI FORMATION IN HULUSTAI MINE DISTRICT OF THE NORTH HELANSHAN COAL FIELD |
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| ZHONG Rong,CHEN Zhong-hui,FU Ze-ming and YANG Nian-hou.NOTE ON SEDIMENTARY FACIES AND SEDIMENTARY MODELS OF THE MIDDLE AND LOWER SHANXI FORMATION IN HULUSTAI MINE DISTRICT OF THE NORTH HELANSHAN COAL FIELD[J].Acta Geoscientia Sinica,1981,3(1):31-45. |
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| Authors: | ZHONG Rong CHEN Zhong-hui FU Ze-ming and YANG Nian-hou |
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| Institution: | Institute of Geomechanics, Chinese Academy of Geological Sciences;Wuhan College of Geology;Wuhan College of Geology;Coal Prospecting Company of Neimonggol |
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