| 庙前井田童子岩组与文笔山组地层的划分 |
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| 引用本文： | 柳应宁.庙前井田童子岩组与文笔山组地层的划分[J].中国西部科技,2014(6):21-22. |
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| 作者姓名： | 柳应宁 |
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| 作者单位： | 福建省196煤田地质勘探队,福建沙县365500 |
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| 摘 要： | 福建庙前井田属福建二叠纪含煤地层连城区,童子岩组的第一段、第二段的沉积特征与文笔山组相似,均为黑灰色泥岩、粉砂岩,地层难以划分,特别是出现缓断层构造时无法进行对比。野外工作中,笔者在文笔山组地层中发现假海乐菊石幼年种这一标志,作为划分依据。
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| 关 键 词： | 二叠纪童子岩组 文笔山组 假海乐菊石幼年种 |
Tungtseyan Formation and Wenbishan Formation to the stratigraphic division in the well-field of Miaoqian,Fujian |
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| LIU Ying-ning.Tungtseyan Formation and Wenbishan Formation to the stratigraphic division in the well-field of Miaoqian,Fujian[J].Science and Technology of West China,2014(6):21-22. |
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| Authors: | LIU Ying-ning |
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| Institution: | LIU Ying-ning(No. 196 Coal Geological Team of Fujian Province, Shaxian, Fujian, 365500, China) |
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| Abstract: | The well-field of Miaoqian belongs to Permian System coal measures in the west of Fujian, and the coal-bearing strata in first and second section of Tongziyan formation are the same as Wenbishan formation. The Pseudohalorites Jurentutis sp. Found in this area was a division basis. |
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| Keywords: | The Permian Tongziyan Formation Wenbishan Formation Pseudohalorites Jurentutis sp |
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