1125年兰州7.0级地震形变破裂带特征及有关问题的讨论  

DISCUSSION ON THE CHARACTERISTICS OF THE FRACTURE ZONE OF THE LANZHOU M7. OEARTHQUAKE IN 1125 AND THE PROBLEMS CONCERNED

作　　者：何秀琴[1] 王多杰[1] 万夫领 

机构地区：[1]国家地震局兰州地震研究所,兰州730000

出　　处：《华北地震科学》1997年第1期37-44,共8页North China Earthquake Sciences

摘　　要：根据大量的野外现场考察资料，对1125年兰州7．0级地震形变破裂带的特征以及庄浪河断裂带晚第四纪以来的活动性进行了初步研究，探讨了该次地震的宏观震中位置及其构造背景。并在古地震破裂形迹分析的基础上，运用年代学资料，对庄浪河断裂带全新世以来的古地震事件等问题作了讨论。Based on a vast amount of data of field investigations, this paper preliminarily studies the characteristics of surface rupture zone of the Lanzhou M 7. 0 earthquake in 1125 and the activity features of the Zhuanglanghe fault since late Quaternary, and probes the structural background and macroseismic epicenter of the earthquake. Paleoearthquakes events along the Zhuanglanghe fault since Holocene period,etc. are discussed on the basis of analyzing the traces of paleoearthquakes.Subjectwords: Lanzhou ; earthquake ; surface rupture zone ; paleoearthquake

关 键 词：活断层 全新世 古地震 地震 破裂带 

分 类 号：P315.2[天文地球—地震学]