沉积环境控制下的页岩岩相组合类型及测井表征:以松辽盆地古龙凹陷青山口组为例*
庞小娇1,2, 王贵文1,2, 匡立春1,2, 赵飞1,2, 李红斌1,2, 韩宗晏1,2, 白天宇1,2, 赖锦1,2

Logging evaluation of lithofacies and their assemblage under control of sedimentary environment:a case study of the Qingshankou Formation in Gulong sag,Songliao Basin
PANG Xiaojiao1,2, WANG Guiwen1,2, KUANG Lichun1,2, ZHAO Fei1,2, LI Hongbin1,2, HAN Zongyan1,2, BAI Tianyu1,2, LAI Jin1,2
松辽盆地古龙凹陷青山口组3种纹层结构分类 A—纹层状,Z井,2500.4 m;B—纹层状,Z井,2488.8 m;C—纹层状,Z井,2488.3 m;D—层状,Z井,2481.8 m;E—层状,Z井,2485.3 m;F—层状,Z井,2489.2 m;G—块状,Z井,2512.8 m;H—块状,Z井,2396.5 m;I—块状,介形虫灰岩, Z井,2491.7 m