茅山地区新构造运动的特征  

THE CHARACTERISTICS OF NEO-TECTONIC ACTIVITY IN MAOSHAN REGIONS

作　　者：竺清良[1] 孙寿成[1] 裘然忠 朱永正[1] 秦承昌 李端璐[1] 杨绍武[1] 

机构地区：[1]江苏省地震局 [2]中国科学院南京古生物研究所

出　　处：《地震学刊》1989年第2期74-79,共6页Journal of Seismology

摘　　要：本文具体论述了茅山地区包括茅山山脉和它所控制的直溪桥—桠溪港断陷盆地新构造运动的多种表现形式及其特征以及历史地震活动.笔者在文中后面引用了朱格利奥瑞尼的"复楔状推覆构造"模式,对茅山地区新构造及茅山地区断裂构造的力学成因进行了解释.This paper recounts the various types and characteristics of Neo-tectonic movement as well as the seismicity in the Maoshan and Zhi xiqao-Yaxigang tectonic oasin regions dominated by it. The authors have interpreted the Neo-tectonic movement phenomena and mechanics propery of fault structures in Maoshan and its adjacertt regions by means of the model of complex sphertoidal nappe tectonics (by Migliorini).

关 键 词：新构造运动 地震活动 断裂 茅山 

分 类 号：P546[天文地球—构造地质学]