贵州中部的开阳、瓮安、湄潭、黄平、余庆等县一带,分布着若干个大小不等的“红盆”,系以角度不整合覆于底盘(中生代以前地层)之上的一套白垩系陆相红色砂、砾岩层。这套地层遭受断裂切错的事实,已经清晰地标绘在有关1:20万地质图幅和1:50万贵州省地质图之上。己公布的资料(如1:20万区凋报告及吉汝安;李兴中、韩宝智等的文章)对于这类新生代发育的断裂亦曾有所论及。 Central Guizhou Kaiyang, Weng’an, Meitan, Huang Ping, Yu Qing counties around the distribution of a number of different sizes, “Red Basin” Department of the angle of unconformity over the chassis (before the Mesozoic strata) above Set of Cretaceous terrestrial red sand, conglomerate layer. The fact that this formation was subjected to faults and faults has been clearly marked on the 1: 200,000 geological map and 1: 500,000 geological maps of Guizhou Province. Published data (such as 1: 200,000 regional withering reports and articles by Ji Ru’an, Li Xingzhong and Han Baizhi et al.) Have also dealt with this type of break in the development of the Cenozoic.