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.
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