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岩性类型及特征 A—长英质页岩,Y井,2245.3 m;B—黏土质页岩,Y井,2324.84 m;C—上部为长英质页岩下部为黏土质页岩,Y井,2247.2 m;D—介壳灰岩,Y井,2373.86 m;E—黏土质页岩,Z井,2508.4 m;F—长英质页岩,Z井,2491.15 m;G—长英质页岩,Z井,2492.49 m; H—介壳灰岩,Z井,2489.9 m;I—介壳灰岩,Z井,2491.65 m;J—云岩,Z井,2496.28 m;K—鲍马序列,W井,箭头指向底部