中国古老超深层海相碳酸盐岩储集层成因研究新进展*
乔占峰1,2, 于洲1,2, 佘敏1,2, 潘立银1,2, 张天付1,2, 李文正1,2, 沈安江1,2

Progresses on ancient ultra-deeply buried marine carbonate reservoir in China
QIAO Zhanfeng1,2, YU Zhou1,2, SHE Min1,2, PAN Liyin1,2, ZHANG Tianfu1,2, LI Wenzheng1,2, SHEN Anjiang1,2
川中古隆起北斜坡灯影组碳酸盐岩储集层岩石学特征 a—PS2井,7800.97 m,凝块石白云岩; b—PS2井,7797.35 m,叠层石白云岩; c—PS5井,5636.94 m,砂屑白云岩; d—PS2井,7793.94 m, 泡沫绵层石白云岩; e—PS4井,6226.37 m,裂缝型白云岩; f—PS2井,7796.03 m,角砾状白云岩