岩性油气藏 ›› 2021, Vol. 33 ›› Issue (6): 93101.doi: 10.12108/yxyqc.20210610
• 油气地质 • 上一篇
田晓平, 张汶, 周连德, 沈孝秀, 郭维
TIAN Xiaoping, ZHANG Wen, ZHOU Liande, SHEN Xiaoxiu, GUO Wei
摘要: 南堡凹陷古生界潜山为渤海海域重要的油气勘探和评价目标。为研究该构造二号断裂带古生界碳酸盐岩潜山岩溶模式,通过岩心观察、薄片鉴定、测井分析、构造演化、岩溶演化模式等研究,结合古地貌特征对各区块岩溶模式差异性进行了综合分析。结果表明:①岩溶储层岩性为灰岩和白云岩,具有双重孔隙介质特征,其基质孔隙连通性较差,裂缝在储集空间中起到关键作用。一方面可对微观孔隙进行沟通疏导,另一方面沿裂缝发育的溶蚀孔洞为重要的储集空间。②潜山岩溶储层主要经历了表生期岩溶作用和埋藏期胶结作用,其中表生期岩溶受印支—燕山早期逆冲褶皱作用影响,形成了现今构造格局和断裂系统,控制了岩溶储层的发育和分布,但燕山中晚期—喜山期的埋藏胶结为岩溶储层形成过程中的破坏作用,主要表现为地表水和地层水对早先形成的缝洞储集空间进行充填。③岩溶作用强度受古地貌和断裂控制。根据古地貌形态及岩溶作用强度划出岩溶高地、岩溶斜坡区和岩溶洼地,各区块间及同区块内岩溶储层发育程度差异主要是离断层远近、古地貌位置高低和斜坡陡缓的原因造成的。其中靠近断裂的古地貌斜坡缓坡带岩溶作用最强,保存条件最好,岩溶储层最为发育,为油气勘探的有利目标。该研究成果对碳酸盐岩潜山的油气勘探具有指导意义。
中图分类号:
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