石油与天然气地质 ›› 1982, Vol. 3 ›› Issue (4): 395-400.doi: 10.11743/ogg19820421

• 论文 • 上一篇    

茅山地质构造与找油

关士聪   

  1. 地质矿产部科学技术顾问委员会
  • 收稿日期:1982-06-29 出版日期:1982-12-25 发布日期:2012-01-16

GEOLOGICAL STRUCTURES OF MAOSHAN AND ITS OIL PROSPECTING

Guan Shicong   

  1. Advisory Committee of Science and Technology, Ministry of Geology and Mineral Resources
  • Received:1982-06-29 Online:1982-12-25 Published:2012-01-16

PDF (PC)

547

被引次数

8

摘要：

茅山山脉位于江苏省句容、溧水、高淳与金坛、溧阳诸县之间。总体呈北北东向延伸,但在吉山至白马山及云山至北山段,山脉及地层走向转为北东至北东东。以高淳双石牌至溧阳桠溪港一线为界,可分为南北两个 S 形段。北段山脉以东和以西在第四系掩覆下,有巨厚的中、新生代沉积,被分别称为常州(金坛)和句容盆地;南段山脉倾没于宣(城)广(德)南(陵)盆地中。

Abstract:

There were three explanations about the geological structures of Maoshan.First,accustomed saying,Maoshan including the most southern area of Anhui and Ji-angsu was the main range of the foldings formed in Indo-China movement; second, by geomechanics, Maoshan waa considered as a combination of several diffuent struetural systems, the north-south axis of Ningzhen Mt. reflexed are, and too, to be unrooted; third, recently, geologists working in plate-tectonic field emphasized the "listric fault" formed by stresses wmprrssed from cast to west in southun China, and thus Maashan was one of the nappes.