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沉积学报  2015 

珠江口盆地重要不整合界面与珠江沉积体系演化分析

DOI: 10.14027/j.cnki.cjxb.2015.03.017, PP. 587-594

Keywords: 珠江口盆地,不整合,沉积体系演化,陆架边缘三角洲

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Abstract:

以珠江口盆地区域二维地震资料、钻井资料为基础,结合南海扩张演化历史,重点研究了盆地内部重要不整合面、盆地演化以及对珠江沉积体系演化的控制作用,旨在为南海北部珠江沉积体系深水油气勘探提供支持和参考。研究结果表明珠江口盆地除基底外,发育三个重要的不整合面,即破裂不整合、陆坡跃迁不整合和陆坡坡度突变不整合;据此将珠江口盆地珠江沉积体系演化划分为四个阶段裂陷期主要发育河流、湖泊相沉积;断陷陆坡期主要发育陆架边缘三角洲沉积(前积层较陡);拗陷缓陆坡期发育陆架边缘三角洲沉积(前积层较缓);拗陷陡陆坡期主要为三角洲—海底峡谷—海底扇沉积。断陷陆坡期与拗陷缓坡期陆架边缘三角洲的勘探,应沿陆架坡折横向去勘探;而拗陷陡陆坡期三角洲—海底峡谷—海底扇,应采取纵向勘探的思路,垂直于陆架坡折方向寻找油气。

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