江西核电厂帽子山候选厂址区域地壳稳定性研究
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摘要
帽子山候选厂址区域范围绝大部分在扬子准地台范围内。区内深大断裂多分布在二级构造单元的分界线上。大别山、怀玉山、九岭等3个隆起区、鄱阳湖、九江─芜湖等2个沉降区和夹于它们之间的庐江─广济、庐山─梅岭、万年─黄石、北淮阳、铜陵─宁国等构造变形带组成了候选厂址区域范围新构造期的基本构造格局。通过布格异常梯度值、重力异常与高程的相关系数、地壳应变能量、地震震级、地震基本烈度、叠加断裂角等地壳稳定性分级指标的综合分析与对比,候选厂址区域范围可划分为九江─安庆、怀玉山、鄱阳湖、九岭稳定亚区及北淮阳─铜陵、大别山基本稳定亚区。帽子山候选厂址位于九江─安庆稳定亚区内.具备核电厂建设的区域地壳稳定性条件。
Maozishan candidated site of factory is mostly limited within the range of Yangzi paraplatform. Through a composite analysis and correlation of grade index of crustal stability, such as Bouguer anomalous gradient value, the relative coefficent of gravity anomaly and elevation, strain energy, earthquake magnitude, the basic intensity of earthquake and superimposed faulted angle, etc, the regional range of candidated site of factory can be divided into Jiujiang-Anqing, Huaiyushan, Poyang Lake and Jiulingstability subareas and the basic stability subareas of north Huaiyang-Tongling and Dabieshan. The Maozishan candidated site of factory is located within Jiujiang-Anqing stability subarea. So, if is qualified for the regional crustal stability conditions of constructing the nuclear electric plant.
引文
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