摘要
在东汤峪地区已有地质工作的基础上,进一步研究了区内地质构造特征,着重分析了山前断裂的构造特征及演化史,认为山前断裂经历了挤压和拉张交替作用的多期(次)活动过程;并探讨了该区温泉的构造控制因素,认为东汤峪温泉主要由区内山前断裂所控制。
On the basis of the previous geological study on the Eastern Tangyu, the authos made a further study of the geological structure features in the area, and special care is taken in the study of the development course of the piedmont fault in the region. It is thought, that the piedmont faulf kas underwent poly-period activity course of compression and extension,the control factors of hot spring in the research area is also probed. It is concluded that the hot spring in the Eastern Tangyu are primarily controlled by the piedmont fault in the region.
出处
《西安工程学院学报》
2002年第4期9-12,共4页
Journal of Xi'an Engineering University
