摘要
研究了老虎山全新世活动断裂的几何学、运动学、古地震和大震复发间隔等的最新活动状况，应用第四纪研究的最新成果，较好地解决了老虎山地区第四纪微地貌的年代问题，并获得了可靠的活动断裂参数。
The Laohushan fault is a Holocen active fault. In thie paper, its geometry, kinematics,paleo earthquakes and recurrence interval of great earthquakes are disscussed. In order to obtain the reliable slip rate of the fault, the new achievement in the research of Quatenary climatology has been introduce into microgeomorphologic dating.
出处
《华南地震》
1994年第4期9-16,共8页
South China Journal of Seismology
基金
国家地震局合同制项目
关键词
活动断裂
古地震
古气候
古土壤
老虎山地区
Active fault activity,Paleoearthquake,Microgeomorphology,Paleoclimate,Paleosoil
