岩性油气藏 ›› 2025, Vol. 37 ›› Issue (2): 153165.doi: 10.12108/yxyqc.20250214
• 地质勘探 • 上一篇
徐兆辉1, 曾洪流2, 胡素云1, 张君龙3, 刘伟1, 周红英1, 马德波1, 傅启龙2
XU Zhaohui1, ZENG Hongliu2, HU Suyun1, ZHANG Junlong3, LIU Wei1, ZHOU Hongying1, MA Debo1, FU Qilong2
摘要: 塔里木盆地轮探1井揭示深层下寒武统白云岩具备油气勘探潜力,古城地区与轮探1井位于同一台缘带。利用地震沉积学的地震地貌学和地震岩性学两大分支学科原理研究了古城地区下寒武统沉积特征,将相位旋转、小波分频、wheeler域转换、地层切片和RGB融合技术整合,形成了地震地貌学(模式驱动)研究流程,从而定性表征沉积相;将相位旋转、小波分频、地震属性提取、主因子分析和随机拟合技术整合形成了地震岩性学(数据驱动)研究流程,从而定量预测储层分布。研究结果表明:①塔里木盆地古城地区下寒武统自西向东发育内缓坡、中缓坡、外缓坡至盆地环境,组成完整沉积相序。中缓坡发育3套(6期)礁滩体,第2套受后期潮道改造,形成潮道改造型碳酸盐岩颗粒滩,潮道内地层较均质,潮道间地层垂向非均质性强导致地震频率较高。②研究区外缓坡近端发育线物源斜坡扇,外缓坡远端至盆地区域发育点物源盆底扇。源自中缓坡礁滩体系的沉积物沿着同沉积走滑断裂相关峡谷被搬运,从而形成了斜坡扇和盆底扇。③研究区储层多发育于中缓坡,外缓坡至盆地较少,内缓坡几乎不发育。外缓坡至盆地区域发育的斜坡扇和盆底扇、中缓坡发育的潮道间岩溶颗粒滩和潮道口发育的潮汐三角洲储层厚度较大。
中图分类号:
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