| 屯溪地区震旦纪岩相古地理研究 |
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| 引用本文： | 彭花明.屯溪地区震旦纪岩相古地理研究[J].华东地质学院学报,1996,19(4):382-386. |
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| 作者姓名： | 彭花明 |
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| 作者单位： | 华东地质学院地科系 |
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| 摘 要： | 安徽屯溪地区震旦系下统碎屑岩系和上统碳酸盐，硅质沉积岩组成，沉积相序由河流相，滨海相，陆棚相和深水盆地相组成，反映了裂陷盆地的特征。
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| 关 键 词： | 沉积序列 岩相古地理 震旦纪 |
The Study of Sinian Sedimentary Facles and Paleogeography in Tunxi Region |
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| Peng Huaming.The Study of Sinian Sedimentary Facles and Paleogeography in Tunxi Region[J].Journal of East China Geological Institute,1996,19(4):382-386. |
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| Authors: | Peng Huaming |
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| Abstract: | The sinian is composed of elastic rocks and carbonate and siliceous sedmentary in Tunxi. It has river factes lihoral factes shelf factes and profundal basin factes. And these show us that the basin is a rift depressive basin. |
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| Keywords: | sedimentary sequence sedimentary facies and palaeogeography sinian period Anhui Tunxi |
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