The Meso Cenozoic basin in Anhui Henan border area is located in the south of Hefei basin.
豫皖交界地段中新生代盆地位于合肥盆地的南缘。
The southwest foreland basins in Tarim Basin is composed of Paleozoic basins and the Meso Cenozoic foreland basins.
塔西南前陆盆地是古生代克拉通盆地与中、新生代前陆盆地的复合，在剖面上呈向北抬升的箕状结构。
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。
应用推荐