岩性油气藏 ›› 2023, Vol. 35 ›› Issue (1): 1224.doi: 10.12108/yxyqc.20230102
文华国1,2, 罗冰3, 钟克修3, 冯青平3, 刘磊1,2, 廖义沙3, 彭才4, 蔡家兰3, 徐文礼1,2, 朱宜新3, 郝静3, 罗鑫3, 徐姁3
WEN Huaguo1,2, LUO Bing3, ZHONG Kexiu3, FENG Qingping3, LIU Lei1,2, LIAO Yisha3, PENG Cai4, CAI Jialan3, XU Wenli1,2, ZHU Yixin3, HAO Jing3, LUO Xin3, XU Xu3
摘要: 地质历史时期的构造-沉积分异作用对大型含油气盆地内碳酸盐岩层系的沉积充填过程及成藏地质条件具有重要影响。通过覆盖全区的二维地震及钻测井资料,对川东地区三叠系嘉陵江组沉积时期隆凹格局及古地理演化进行了精细刻画。研究结果表明: ①从地震剖面、地层及岩性组合等特征上识别出邻水-丰都台凹,其两侧坡度为 1°~2°,且左侧坡度大于右侧坡度;②邻水-丰都台凹与其他古地质单元共同控制了嘉二段沉积时期川东地区的古地理格局及构造-沉积分异特征,嘉二段沉积早-中期,颗粒滩沿邻水-丰都台凹周缘发育,晚期台凹内则大面积发育膏质潟湖沉积;③邻水-丰都台凹及周缘微古地貌控制沉积早期颗粒滩分布,台凹周缘地貌高部位更易形成优质白云岩储层,持续干旱、蒸发环境致使沉积晚期台凹内形成区域盖层沉积;④总体来看,嘉二段具备良好的成藏地质条件,有望成为寻找滩相整装气藏的战略勘探层系,建议将邻水-丰都台凹周缘台内滩相发育带作为川东地区嘉陵江组下步勘探重点区之一。
中图分类号:
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