1668年郯城8.5级地震断裂的全新世滑动速率、古地震和强震复发周期
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HOLOCENE DISPLACEMENT RATE, PALEOEARTHQUAKES AND RECURRENCEINTERVALS OF STRONG EARTHQUAKES ALONG THE 1668 TANCHENGEARTHQUAKE (MS=8.5) FAULT
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    摘要:

    本文根据野外考察、实测和开挖资料研究了1668年郯城8(1)/(2)级地震断裂上的全新世位移分布、滑动速率、古地震遗迹、古地震期次和强震复发周期以及地震破裂模式。

    Abstract:

    Based on data of author's field investigating, measuring and trenching, the distribution and rate of Holocene displacement, paleoearthquake's traces and times, recurrence intervals of strong earthquakes (Ms=8-8.5) and model of the earthquake fracture along the 1668 Tancheng earthquake fault are studied in the paper.

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王华林.1668年郯城8.5级地震断裂的全新世滑动速率、古地震和强震复发周期[J].地震工程学报,1995,17(4):1-12,22. Wang Hualin. HOLOCENE DISPLACEMENT RATE, PALEOEARTHQUAKES AND RECURRENCEINTERVALS OF STRONG EARTHQUAKES ALONG THE 1668 TANCHENGEARTHQUAKE (MS=8.5) FAULT[J]. China Earthquake Engineering Journal,1995,17(4):1-12,22.

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  • 收稿日期:1995-01-24
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  • 在线发布日期: 2017-06-30