鲁西豫东地区奥陶系岩溶热储形成演化及主控因素分析*
隋少强1,2, 杨志波3,4, 赵雅静3,4, 贾艳雨1,2, 宿宇驰3,4, 王茜1,2, 高飞1,2, 季汉成3,4, 鲍志东3,4

Evolution and main controlling factors of the Ordovician karst thermal reservoir in western Shandong-eastern Henan area
SUI Shaoqiang1,2, YANG Zhibo3,4, ZHAO Yajing3,4, JIA Yanyu1,2, SU Yuchi3,4, WANG Xi1,2, GAO Fei1,2, JI Hancheng3,4, BAO Zhidong3,4
鲁西豫东地区奥陶系碳酸盐岩储集空间类型 a—粒间孔(图中箭头方向),鲕粒灰岩,黄古1井,2194 m,下马上,单偏光; b—溶蚀孔,粉晶白云岩,毛4井,2580.45 m,峰峰组上,单偏光; c—晶间孔,晶粒云岩,×1400,龙古2井,1284.0 m,峰峰组下; d—高角度缝(黄色箭头方向),泥粉晶白云岩,含膏质,范古2井,2906 m,峰峰组下; e—构造缝(图中箭头方向),生屑灰岩,毛4井,2592.5 m,峰峰组上,单偏光; f—构造—溶蚀缝,方解石、沥青质充填,毛4井,2731.5 m,峰峰组下; g—缝合线,沥青质充填(图中箭头方向),晶粒灰岩,毛4井,2587.19 m,峰峰组上,单偏光; h—溶蚀洞,风化壳作用,高1井,1441 m,下马上