摘要
本溪水洞位于上马家沟组砾屑灰岩中。洞穴的形成主要受北西向断裂构造控制，当时的古气候、古地貌以及水文地质条件是其形成的重要因素。水洞形成于中－晚更新世。
The development of Benxi water cave in the pebble limestone of the Upper Majiagou Fermation is initially contralled by a group of faults in NW direction. The paleo climate, paleo geography and underground water, are also among the most importent factors contributing to the formation of the cave. It is indicated that the main cave was formed in middle pleistocene to Late pleistocene.
出处
《长春科技大学学报》
CSCD
1998年第2期148-152,共5页
Journal of Changchun University of Science and Technology
