Most of the uranium deposits in China occurs in geological setting of the geosynclinal folded zone and the mobile region, and hydrothermal uranium deposits are dominant position.
中国铀矿床大多产于地槽褶皱带和活化区地质背景中,以热液铀矿床占主导地位。
The south Dongsuqi is located in the geosynclinal fold system of Middle Inner Mongolia.
东苏旗南部处于内蒙古中部地槽褶皱系。
Some endogenetic gold deposits controlled by the fold systems which situated in the pre geosynclinal and the geosynclinal stages are formed in the Meso Cenozoic eras also.
一些于前地槽、地槽阶段形成的褶皱构造体系所控制的内生金矿产,在形成时代上也属于中-新生代。
In recent years, there more different types mo deposits (spots) have been discovered in Jilin geosynclinal area, mainly porphyry, quartz vein, skarn and fracture altered rock deposits.