断层崖形成年代的数学模拟计算
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国家地震局地震科学联合基金


MATHEMATICAL MODEL CALCULATION OF FAULT SCARP AGE
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    摘要:

    本文在对物质扩散方程进一步推导的基础上,分别用数学方程模型Ⅰ、Ⅱ、Ⅲ对发育在昌马断裂带中、东段的单一型地震断层崖和复合型地震断层崖剖面进行了拟合计算。并用最大坡值-断距(tgθs-2a)图分析了阿尔金断裂带和昌马断裂带上分布的离散型断层崖。结果求得:昌马断裂带断层崖的物质扩散系数K值为2.1~3.4m2/103a。阿尔金断裂带上发育有4组距今年龄分别为0.6ka、2-2.7ka、4ka和6-6.6ka的地震断层崖。

    Abstract:

    On the basis of further deduction of diffusion equation,the profiles of single-shock and multi-shock fault scarps along middle and eastern segments of Changma fault zone are fitted and calculated by using mathematical equation models Ⅰ,Ⅱ and Ⅲ. The disperse fault scarps along the Altun fault zone and Changma fault zone are analyzed by using the maximum slope value-fault throws(tgθs-2a)pattern. The results show that for the fault scarps of Changmafault zone the mass diffusion coefficient K=2.1-3.4m2/103 a and along Altun fault zone there are 4 sets of seismic fault scarps whose ages are 0.6 ka,2-2.7 ka, 4ka and 6-6. 6 ka respectively.

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侯康明,韩有珍,张守杰.断层崖形成年代的数学模拟计算[J].地震工程学报,1995,17(2):68-75,81. Hou Kangming, Han Youzhen, Zhang Shoujie. MATHEMATICAL MODEL CALCULATION OF FAULT SCARP AGE[J]. China Earthquake Engineering Journal,1995,17(2):68-75,81.

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  • 在线发布日期: 2017-06-30