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埋藏溶蚀特征 a—硅质灰岩,硅质热液流体沿裂缝侵入,碳酸盐岩硅化,龙古3井,2329.8 m;b—角砾灰岩,发育X型裂缝,硅质充填, 范古2井,2906.54 m;c—泥晶灰岩,沿裂缝发育溶蚀阔缝,有机质充填,马古5井,3356.50 m,正交光;d—泥晶灰岩, 埋藏压溶,溶蚀缝合线发育,文古1井,4799.38 m,单偏光