宁夏六盘山盆地中新生代地质演化研究OACHSSCDCSTPCD
A Research on Geological Evolution of Mesozoic-Cenozoic of Liupanshan Basin in Ningxia
六盘山是宁夏最大的中、新生代沉积盆地,经历了复杂的地质演化过程,根据盆地的野外地质观察资料和已有工作的成果,对六盘山盆地沉积层序、岩性特征、沉积环境及地质构造进行了综合对比研究,将六盘山盆地中、新生代划分为3个演化阶段,其中在三叠纪至侏罗纪期间是盆地初始形成阶段,经历主体抬升,逆冲推覆构造体系得到充分的发展,并与盆地北部形成小型山间,白垩纪盆地北部小型山间合而为一,盆地沉积中心逐渐向南迁移,盆地进入独立演化发育阶段.新生代为盆地改造期,盆地西缘的…查看全部>>
As the largest Mesozoic-Cenozoic sedimentary basin in Ningxia, Liupanshan Mountain has experienced a complicated process of geological evolution. According to the filed geological observation data of basin and the results of previous research done by other people, Liupanshan Basin is divided into three evolution stages based on the comprehensive analysis of its sedimentary sequence, lithologic characteristics, sedimentary environment and geological str…查看全部>>
宗立一;李陇堂;温万成;李园;李卿
宁夏地质博物馆,宁夏银川 750002宁夏大学资源环境学院,宁夏银川 750021宁夏地质博物馆,宁夏银川 750002宁夏地质博物馆,宁夏银川 750002宁夏地质博物馆,宁夏银川 750002
天文与地球科学
六盘山盆地沉积特征地质演化中新生代
Liupanshan Basin sedimentary characteristics geological evolution Mesozoic-Cenozoic
《宁夏大学学报(自然科学版)》 2012 (2)
214-219,6
宁夏自然科学基金资助项目(NZ10205)
评论