高岭石、大部分菱铁矿、黄铁矿、硅质自生矿物及少部分方解石反映了陆相环境。
Kaolinite, a number of siderites, pyrites, siliceous authigenic minerals and a few calcites represent continental environment.
东部沉积微相条件变差，孔洞被亮晶方解石、渗流白云石、硅质等强充填，但以亮晶方解石充填为主。
Microfacies become variation in eastern, pore space are filled by calcsparite, leakdolomite, kiesel and so on. But the main filling is calcsparite.
东部沉积微相条件变差，孔洞被亮晶方解石、渗流白云石、硅质等强充填，但以亮晶方解石充填为主。
Microfacies become variation in eastern, pore space are filled by calcsparite, leakdolomite, kiesel and so on. But the main filling is calcsparite.
应用推荐