超压背景下中深层砂岩储集层沉积—成岩演化差异性分析: 以南海莺歌海盆地中新统黄流组为例*
毛倩茹1, 范彩伟2, 罗静兰1, 曹江骏1, 尤丽2, 符勇1, 李珊珊2, 史肖凡1, 吴仕玖2

Analysis of sedimentary-diagenetic evolution difference on middle-deep buried sandstone reservoirs under overpressure background: a case study of the Miocene Huangliu Formation in Yinggehai Basin,South China Sea
Mao Qian-Ru1, Fan Cai-Wei2, Luo Jing-Lan1, Cao Jiang-Jun1, You Li2, Fu Yong1, Li Shan-Shan2, Shi Xiao-Fan1, Wu Shi-Jiu2
南海莺歌海盆地东方区与乐东区黄流组储集层岩石类型 Ⅰ—石英砂岩;Ⅱ—长石石英砂岩;Ⅲ—岩屑石英砂岩;Ⅳ—长石岩屑石英砂岩;Ⅴ—长石砂岩;Ⅵ—岩屑长石砂岩;Ⅶ—长石岩屑砂岩;Ⅷ—岩屑砂岩