摘要
本文根据野外考察、实测和开挖资料研究了１６６８年郯城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。
Based on data of author's field investigating, measuring and trenching, the distributionand rate of Holocene displacement, paleoearthquake's traces and times, recurrence intervals ofstrong earthquakes (Ms = 8-8.5) and model of the earthquake fracture along the 1668Tancheng earthquake fault are studied in the paper.
出处
《西北地震学报》
CSCD
1995年第4期1-12,22,共13页
Northwestern Seismological Journal
关键词
古地震
复发周期
地震破裂
位移
滑动
震级
Tancheng-Lujiang seismotectonic zone, Palaeoearthquake, Earthquakerecurrence period, Seismic rupture, Displacement, Slip Fujian-Jiangxi Exploring Institutde for Seismogeology-Engineering, Seismological Bureau of Fujian Province,Fuzhau
