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准同生与表生岩溶特征 a—生屑灰岩,针状溶蚀孔,明古1井,3482.0 m;b—泥晶灰岩,膏质铸模孔,东古1井,2403 m,单偏光;c—灰质白云岩,粒间溶孔,黄古1井,2200.5 m,单偏光;d—生屑灰岩,格架孔,马古6井,3099.66 m,单偏光;e—岩溶角砾风化壳,高1井, 1130.57 m;f—溶蚀微裂缝,龙古3井,1652.5 m,峰峰组上段