摘要
鲁西广泛发育NW和NEE向两组断裂。通过该两组断裂特征和演化的研究,再造不同时期的构造应力分布,区分出中生代以来的五期构造应力场。各期构造应力的作用方向。
In Western Shandong, faults in NW and NEE trend developed very well. In this paper, the authors reconstructed the distribution of tectonic stress in different periods and identified the existance of five periods of tectonic stress fields through the study of the features and evolution of the two groups of faults. The source of driving forces for the acting direction of the tectonic stresses in different periods can be found from the plate tetctonic movement
出处
《山东矿业学院学报》
CAS
1989年第4期18-25,共8页
Journal of Shandong University of Science and Technology(Natural Science)
关键词
地质构造
应力场
板块运动
新生代
geological structure
field of stress
tectonic development history
geological fracture
