吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (6): 1589-1596.doi: 10.13278/j.cnki.jjuese.201506103
张宇焜, 胡晓庆, 牛涛, 张显文, 高玉飞, 王晖, 范廷恩, 卜范青
Zhang Yukun, Hu Xiaoqing, Niu Tao, Zhang Xianwen, Gao Yufei, Wang Hui, Fan Ting'en, Bu Fanqing
摘要:
渤海湾盆地石臼坨凸起沙一、二段所发育的扇三角洲储层,在沉积演化过程中由于古地貌特征的不同,造成储集砂体形态特征及分布规律的不同,储层认识困难。通过分析断裂活动对古地貌格局的控制作用进行古地貌恢复,研究不同地貌单元与沉积体系的匹配关系,阐明了古地貌对沉积体系发育类型和沉积特征的控制作用,揭示了扇三角洲的沉积过程。在此基础上结合地震属性分析技术,精细描述了各沉积期次扇体的展布特征,并对沉积演化过程中扇三角洲沉积体系发育的差异性进行了解析。最终明确了盆地边缘沟谷和古地形发育特征对物源的控制作用,形成了"大沟对大扇,小沟对小扇"的沉积模式指导依据;同时确定了斜坡带上扇三角洲的沉积规律和砂体分布的控制机理。
中图分类号:
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