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荧光薄片及含烃包裹体荧光特征 a—DF13-1B井,2870.9 m,发育第1、2期烃类充注;b—DF13-1B井,2870.8 m,发育第2、3期烃类充注;c—DF13-2C井,3297.0 m,发育第2、3期烃类充注;d—LD10-1C井,4039.0 m,发育第1、2、3期烃类充注;e—LD10-1A井,4168.7 m,发育第1、3期烃类充注; f—LD10-1B井,4401.5 m,发育第3期烃类充注。 红色方框中为具有荧光特征的含烃包裹体