白云岩-蒸发岩共生体系白云石化过程研究:以鄂尔多斯盆地马家沟组为例*
吴宇婷1,2,3, 甯濛1,2,3, 夏攀1,2,3, 乔占峰4,5, 于洲4,5, 文华国1,2,3

Research on dolomitization process in dolomite-evaporite syngenetic system of the Majiagou Formation in Ordos Basin
WU Yuting1,2,3, NING Meng1,2,3, XIA Pan1,2,3, QIAO Zhanfeng4,5, YU Zhou4,5, WEN Huaguo1,2,3
鄂尔多斯盆地西磑口剖面马家沟组白云岩宏观及微观特征 A—浅黄色厚层白云岩,刀砍纹发育,S1段底部; B—膏溶角砾白云岩,S1段,1.2 m;C—膏溶角砾白云岩,S1段,5.2 m;D—颗粒白云岩,S2段,31.1 m;E—泥晶白云岩,可见水平纹层状构造,单偏光,S1段,2.9 m;F—泥晶白云岩,发育大量石膏假晶,后期被方解石交代,单偏光,S1段,1.4 m;G—膏溶角砾白云岩,可见由泥晶白云石构成的“角砾状”构造,发育石膏假晶,单偏光,S1段,2.7 m;H—内碎屑颗粒白云岩,可见由泥晶白云石构成的砂屑颗粒,颗粒具有定向性,单偏光,S1段,5.2 m;I—细晶白云岩,溶蚀孔隙发育,单偏光,S2段,23.3 m;J—细晶白云岩,裂缝和溶蚀孔隙发育,单偏光,S2段,27.8 m;K—泥晶白云岩,发育少量石膏假晶,单偏光,S2段,29 m;L—泥晶白云岩,发育裂缝和少量石膏假晶,单偏光,S2段,29.35 m;M—颗粒白云岩,可见由泥晶白云石构成的砂屑颗粒,颗粒间的胶结物发生白云石化,单偏光,S2段,28.7 m