生物碎屑灰岩差异成岩及储集层特征:以伊拉克HF油田白垩系Mishirif组为例*
余义常1, 宋新民1, 郭睿1, 高兴军1, 林敏捷1, 衣丽萍1, 韩海英1, 陈军2, 邓亚1, 李峰峰1, 刘航宇3

Differential diagenesis and reservoir characteristics of bio-clastic limestone: A case study on the Cretaceous Mishrif Formation in HF Oilfield,Iraq
Yu Yi-Chang1, Song Xin-Min1, Guo Rui1, Gao Xing-Jun1, Lin Min-Jie1, Yi Li-Ping1, Han Hai-Ying1, Chen Jun2, Deng Ya1, Li Feng-Feng1, Liu Hang-Yu3
伊拉克HF油田Mishrif 组岩石类型 a—N195井,3001.4~3001.6im,具水平层理的泥晶灰岩;b—N195井,3034.5~3034.7im,具生物扰动的粒泥灰岩;c—Y161井,2934.4~2934.6im,具低角度交错层理的泥粒灰岩;d—Y161井,3002.5~3002.7im,具平行层理的颗粒灰岩