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).
出处
《地震学刊》
CSCD
1989年第2期74-79,共6页
Journal of Seismology
