摘要
本文初步研究了郯庐断裂带泗洪孙牌坊区段全新世时期的活动性。利用地质剖面开挖、地质填图、取样分析、土氡测量等手段,获取了较多资料,证实了泗洪段全新世以来有活动。
This paper studied the activity along the Sihong segment of Tanlu fault zone during Ho-locene. More data obtained from the geological profile excavation, geological mapping, sampling analysis and soil radon measurement confirm that there has been recent activity along the Sihong segment since Holocene.
出处
《地震》
CSCD
北大核心
1992年第5期61-64,71,共5页
Earthquake
