地震地磁观测与研究2024，Vol.45Issue(1)：13-22,10.DOI:10.3969/j.issn.1003-3246.2024.01.002
滦县—卢龙断裂的活动特征及其地震地质意义
The characteristics of activity of the Luanxian-Lulong fault and its seismic geological significance
摘要
Abstract
This paper studies the activity characteristics and seismic geological significance of Luanxian-Lulong fault by combining field surface geology and geomorphological survey,shallow artificial seismic reflection exploration and trough exploration.The Luanxian-Lulong fault is located in Luanxian and Lalong,generally towards NNE-NE,inclined W,with inclination of 60-70,and it is a reverse fault with 2-3 km wide and about 31 km long.The fault controls the development of Luanhe River Valley and its tributaries in some sections.Along the fault,there exists dynamic deterioration and forms obvious fault trough valley landform.According to the comprehensive means of shallow artificial seismic exploration,trough exploration,regional stratigraphic comparison and dating,it caused the deformation of quaternary strata,which was the active fault in the late Pleistocene.Although the Luanxian-Lalong fracture deformation is weak,the discussion believes that this can not rule out the possibility of strong earthquake in the future.关键词
滦县—卢龙断裂/构造变形/活动特征/晚更新世断裂Key words
Luanxian-Lulong fault/structural deformation/activity characteristics/late Pleistocene fault引用本文复制引用
刘燕翔,王晓山,吕国军,茅远哲,边庆凯,荣伟健..滦县—卢龙断裂的活动特征及其地震地质意义[J].地震地磁观测与研究,2024,45(1):13-22,10.基金项目
唐山市滦县—乐亭、卢龙—滦县断裂活动性鉴定及定位项目 （）
河北省地震科技星火计划项目(项目编号:DZ2021121700006) （项目编号:DZ2021121700006）
