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用地震断层陡坎的形态方程确定古地震事件的年代

USING THE SHAPE EQUATION OF SEISMIC FAULT STEP TO DETERMINE THE CHORN OF AN EARTHQUAKE EVENT
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摘要 通过对地震断层陡坎演变过程的分析,应用均匀物质扩散理论建立地震断层陡坎的形态方程,推断古地震断层陡坎的年龄,从而确定古地震事件的期次及年代。用该方法对二台活断层古地震断层陡坎进行计算,所得结果与用其它方法确定的古地震事件的期次及年代对应较好。 Based on the analysis of evolutionary process of seismic fault step,the shape equation ofseismic fault step was built by applying uniform matter diffusion theory- Using the equationcan obtain the age of a paleoearthquake fault step,thus determining the chorn and perlod-time of the paleoearthquake. The paleoearthquake step on Ertai active fault was taken as anexample in this paper;its chorn and period-time were drawn from the shape equation.whichis corresponding to the results from other methods very well.
出处 《内陆地震》 1997年第2期148-153,共6页 Inland Earthquake
关键词 断层陡坎 古地震 断裂 地震 形态方程 fault scarp Palaeoearthquake Ertai fault Xinjiang
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参考文献1

  • 1张裕明.可可托海—二台断层陡坎的坡角变化、年龄和大地震重复时间间隔[J]中国地震,1986(01).

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