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| THE NEOTECTONIC MOVEMENT AND THE CHANGE OF WATER SYSTEM IN THE REGION OF HAIZHOU BAY |
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| Our study indicates that the rifts of Xiangshui, Yishu and Jiaonan edged the region of Haizhou Bay with distinct boundary. This region, with the second-class rifts lying northeast and northwest, shows its structure of fault block clearly. Because of the obvious neotectonic movement and its variation in this region, the relief was higher in the northwest and lower in the southeast, with the Mount Yuntai being raised as a fault block, hence the coast and surface water system were changed. |
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