高频基准面旋回控制下浅水三角洲及其砂体发育模式:以松辽盆地扶余油田白垩系泉头组为例*
赖洪飞1,2, 秦智3, 王洪君3, 郑锡3, 林艳波3, 鲍志东1,2, 李美俊1,2, 张云龙1,2, 张莉1,2, 吴煜潇1,2, 宋健1,2, 何陵沅1,2

Development pattern of shallow-water delta and sandbodies under control of high-frequency base-level cycles: A case study of the Cretaceous Quantou Formation in Fuyu Oilfield, Songliao Basin
Lai Hongfei1,2, Qin Zhi3, Wang Hongjun3, Zheng Xi3, Lin Yangbo3, Bao Zhidong1,2, Li Meijun1,2, Zhang Yunlong1,2, Zhang Li1,2, Wu Yuxiao1,2, Song Jian1,2, He Lingyuan1,2
松辽盆地扶余油田DT91区块白垩系泉头组泉四段第Ⅲ砂组超短期基准面旋回类型 A—单河道砂体,A1型,D60-012井;B—切叠型河道砂体组合,A1型,D54-10.4井;C—单河道砂体,A2型,D+52-18井;D—叠加型河道砂体组合,A2型,D60-12.4井;E—单个分流砂坝,B1型,D+54-10.2井;F—切叠型分流砂坝组合,B1型,D+48-15.2井;G—单个分流砂坝,B2型,D+48-15井;H—叠加型分流砂坝组合,B2型,D+56-10.4井;I—河道—天然堤组合,C1型,D+58-09.2井; J—河道—分流砂坝组合,C2型,D64-17井;K—河道—分流砂坝组合,C3型,D64-17井