山东国土资源2015，Vol.31Issue(12)：27-32,6.
千佛山与趵突泉泉水形成关系研究
Research on Relationship between the Formation of the Baotu Spring and Qianfo Mountain
摘要
Abstract
In this paper, through analysis on the formation of sedimentary covers,magmatic intrusion, development process and evolution of carbonate rocks, cutting and destroying to the cover layers and the formation of landscapes caused by tectonic movement, internal connection of four springs represented by Qianfo Moutain, Fohui Moutain and Baotu Spring has been analyzed. It is showed that late Yanshan movement has established the structures of Ji-nan city, and geomorphic characteristics are similar to now in Qianfo Moutain, Fohui Moutain area were formed in late Neogene, and in the urban areas, roof window came into being around Baotu Springs and Heihu springs. Qian-fo Moutain and Fohui Moutain area are important recharge area of Baotu Spring. Carbonate rocks are hidden in the urban underground, which are important mediators of three types of water transformation system. In low-lying ter-rain and favorable position of tectonics, Baotu spring start gushing out at about ten thousand years to six thousand years ago.关键词
千佛山/趵突泉/碳酸盐岩/燕山运动/天窗/三水转化Key words
Qianfo moutain/Baotu spring/carbonate rocks/Yanshan movement/roof window/three type water transformation分类
天文与地球科学引用本文复制引用
韩连山,汪玉静,韩昱..千佛山与趵突泉泉水形成关系研究[J].山东国土资源,2015,31(12):27-32,6.基金项目
山东地矿重大科技攻关项目( 2012-045) （ 2012-045）
