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bei jing ba bao shan duan lie dai mei ling hu xing di duan xian jin ying li chang de shu xue mo ni
Author(s): 
Pages: 36-40+43
Year: Issue:  4
Journal: Hydrogeology and Engineering Geology

Keyword:  有限单元法边界条件主压应力应力分布断裂组顺时针断层八宝山断裂带数学模拟弹性圆盘;
Abstract: <正> 八宝山断裂带是形成于燕山运动中晚期的一组NE—SW向断裂构造。主要由二条大断裂系统组成,东侧一条(F1)称黄庄—高丽营断裂;西侧一条(F2)为八宝山断裂,它又大体由二条平行相伴的断裂组成,二者相距300—500米。 煤岭弧形断裂地段系指八宝山断裂的西南部分。南邻房山侵入岩体,北近谷积山弧形背斜,具压扭性呈弧形向北西凸出(图1)。
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