岩性油气藏 ›› 2018, Vol. 30 ›› Issue (5): 110.doi: 10.12108/yxyqc.20180501
• 油气地质 • 下一篇
杜晓峰, 王清斌, 庞小军, 代黎明, 张参
DU Xiaofeng, WANG Qingbin, PANG Xiaojun, DAI Liming, ZHANG Can
摘要: 为解决渤中凹陷石南陡坡带东三段砂砾岩储层分布等问题,利用三维地震、钻井、分析化验等资料,对东三段源汇体系中形成砂砾岩的关键要素进行了定量表征。结果表明:①东三段储层主要为扇三角洲砂砾岩,其物源区母岩岩性多样,南部母岩主要为中生界火山岩;西北部母岩为火山岩、碳酸盐岩和花岗岩。②物源区发育5个面积大、延伸远的陡坡沟谷体系,输送了大量的砂砾岩沉积物。③东三段的沉积古地形以断槽型为主,由西向东,断层呈分段式活动,造成了物源和沉积区的差异升降。④砂砾岩的延伸距离与湖平面的升降呈此消彼长的关系,湖平面离物源越近,砂砾岩延伸越近;反之,砂砾岩延伸距离越远。该认识可为断陷盆地陡坡带的砂砾岩储层评价提供依据。
中图分类号:
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