| 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,北部继承性沉降,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。 |
| 关键词: 断块运动 同沉积背斜 济源盆地 |
| DOI： |
| 附件 |
| 投稿时间：1994-03-02 |
| 基金项目: |
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| FAULT-BLOCK MOVEMENT AND EVOLUTION OF THE JIYUAN BASIN DURING THE MESOZOIC |
| Chen Chuanshi,Su Xianbo |
| (Jiaozuo Mining College) |
| 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. |
| Key words: fault-block movement synsedimentary anticline Jiyuan Basin |
