| 休宁白垩系红层盆地的沉积特征和地貌发育 |
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| 引用本文： | 周秉根,吴莉淳.休宁白垩系红层盆地的沉积特征和地貌发育[J].地理研究,1992,11(1):23-29. |
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| 作者姓名： | 周秉根 吴莉淳 |
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| 作者单位： | 安徽师范大学地理系 |
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| 摘 要： | 休宁白垩系红层盆地是晚侏罗纪初,早白垩纪末形成的断陷盆地。盆地形成以后接受白垩纪的红色沉积物,沉积总厚度为2350—3929m。在喜马拉雅运动中盆地抬升,在构造、沉积和外力作用下,形成了典型的红层地貌。
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| 关 键 词： | 休宁盆地 沉积特征 红层地貌 |
| 收稿时间： | 1990-03-17 |
| 修稿时间： | 1991-05-15 |
DEPOSITIONAL CHARACTERISTICS AND GEOMORPHOLOGICAL DEVELOPMENT OF RED STRATUM OF THE CRETACEOUS PERIOD IN THE XIUNING BASIN |
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| Zhou Binggen Wu Lichun.DEPOSITIONAL CHARACTERISTICS AND GEOMORPHOLOGICAL DEVELOPMENT OF RED STRATUM OF THE CRETACEOUS PERIOD IN THE XIUNING BASIN[J].Geographical Research,1992,11(1):23-29. |
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| Authors: | Zhou Binggen Wu Lichun |
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| Institution: | Department of Geography, Anhui Normal University |
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| Abstract: | Xiuning Basin is a fault trough basin.It is situated in the southern part of Anhui Province, China.And its area is 560km2. The regin of the basin was a part of the Jiangnan old continent. During the late Jurassic-early Cretaceous Period, the basin was formed by fault along old fault lines (Proterozic Era) Red sediment was deposited in the basin during the Cretaceous Period and its thickness was 2350-3929m. During the Ximalaya Morement the basin was raised and it was accompanied with fault action. The geomorphological types of red stratum were formed by the tectonic morement, deposition and exogenic force. |
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| Keywords: | Xiuning Basin Depositional characteristics Red stratum geomorphy |
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