| 断块运动与中生代济源盆地的演化 |
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| 引用本文： | 陈传诗,苏现波.断块运动与中生代济源盆地的演化[J].沉积与特提斯地质,1995(1):18-23. |
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| 作者姓名： | 陈传诗 苏现波 |
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| 作者单位： | 焦作矿业学院 |
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| 摘 要： | 晚三叠世，济源盆地南部与北部的岩相古地理面貌及充填特征存在着明显的差异；早中侏罗世盆地南部隆起，北部继承性机降，直到中侏罗世未盆地完全封闭。这种差异是由盆地内部黄河断裂的同沉积活动造成的。
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| 关 键 词： | 断块运动，同沉积背斜，济源盆地 |
| 收稿时间： | 1994/3/2 0:00:00 |
FAULT-BLOCK MOVEMENT AND EVOLUTION OF THE JIYUAN BASIN DURING THE MESOZOIC |
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| Chen Chuanshi and Su Xianbo.FAULT-BLOCK MOVEMENT AND EVOLUTION OF THE JIYUAN BASIN DURING THE MESOZOIC[J].Sedimentary Geology and Tethyan Geology,1995(1):18-23. |
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| Authors: | Chen Chuanshi and Su Xianbo |
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| Institution: | Jiaozuo Mining College |
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| Abstract: | There were remarkable differences in sedimentary facies and palaeogeographic features and filling patterns in the northern and southern parts of the Jiyuan Basin during the Mesozoic.The southern part was uplifted,while the northernone subsided inheritedly during Early and Middle Jurassic time. The basin was completely closed at the end of Middle Jurassic.The differences outlined above are interpreted to be caused by the synsedimentary faulting of the Huanghe fault within the basin. |
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| Keywords: | fault-block movement synsedimentary anticline Jiyuan Basin |
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