岩性油气藏 ›› 2022, Vol. 34 ›› Issue (4): 2231.doi: 10.12108/yxyqc.20220403
李珊珊1, 姜鹏飞2, 刘磊1,3, 雷程4, 曾云贤4, 陈仕臻1,3, 周刚4
LI Shanshan1, JIANG Pengfei2, LIU Lei1,3, LEI Cheng4, ZENG Yunxian4, CHEN Shizhen1,3, ZHOU Gang4
摘要: 四川盆地寒武系沧浪铺组具有良好的成藏地质条件和广阔的勘探前景。通过岩心、三维地震数据、钻测井等资料,利用地质与地球物理相结合,对高磨地区沧浪铺组颗粒滩地震反射特征及沉积特征进行了研究。研究结果表明:①四川盆地高磨地区寒武系沧浪铺组可识别出4种地震反射特征,分别对应4类沉积微相组合,其中强振幅、低频、高连续反射对应的颗粒滩最为发育;②研究区颗粒滩发育于沧一段上部,分布于高磨断裂以东,形态为条带状或不规则状,长轴方向近似平行于古隆起边界,并围绕2个古隆起的翼部呈北东东和北北西方向展布;③沧浪铺组沉积时期,高磨地区整体为浅海陆棚相沉积,发育大量碳酸盐岩颗粒滩,各类颗粒滩的发育及分布主要受海平面变化、沉积期古地貌及物源供给等因素共同控制。
中图分类号:
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