首页|期刊导航|海洋地质前沿|海中凹陷北部陡坡带涠洲组滩坝沉积规律及其主控因素

海中凹陷北部陡坡带涠洲组滩坝沉积规律及其主控因素OA

Sedimentation and controlling factors on beach-bar facies of Weizhou Formation in northern steep slope zone of Haizhong Sag

中文摘要英文摘要

针对海中凹陷北部陡坡带前期三角洲沉积模式与最新钻井认识不符的问题,本文以H3X和H301井为核心,综合岩芯、测井、地震与粒度数据,结合物源、古地貌与古水深约束,重建滩坝沉积体系并分析其主控因素.结果表明,涠洲组普遍发育砂-泥薄互层,箱形/钟形厚层砂体缺失;测井以指形/漏斗形的高频叠置为主;地震相为中—弱振幅、短轴不连续与杂乱/丘状反射,指示典型滩坝特征.结合典型沉积构造与粒度资料,研究区滩坝可划分为沿岸滩坝、近岸滩坝及受风暴影响的远岸滩坝.物源主要来自北侧涠洲油田辫状河三角洲前缘砂体经波浪改造后的远距供砂,并叠加涠西南低凸起基底剥蚀颗粒.沉积期海 3、海 4构造区为水下低隆,3号断裂虽分隔南北沉积格局但未阻断物质跨断裂输运,低隆区成为卸载聚砂带.古生物、波痕参数与相序厚度联合反演显示:水深 0~4 m以沿岸坝为主,水深 4~8 m近岸坝发育,水深8~11 m远岸坝占优.基于此,建立了"物源-古隆起-古水深"共控的滩坝沉积模式,为海中凹陷滩坝型储层识别、主控因素分析与平面预测提供依据,并可推广至同类陆相断陷湖盆.

To address the mismatch between the traditional delta model and new well evidence from the northern steep slope of the Haizhong Sag in Weizhou Formation,Wells H3X and H301 were analyzed by combining core observation,well logging,seismographic facies,and grain-size distribution,with additional constraints from provenance,paleogeomorphology,and paleowater depth,based on which a beach bar-dominated system was re-constructed and its controlling factors were evaluated.Results show that the Weizhou Formation develops vast in-terval sand-mud thin interbeds with no thick box/bell-shaped channel sands.Log responses are dominated by high-frequency finger-and funnel-shaped superimposition motifs.Seismic facies are characterized by moderate-low amplitudes,short-axis discontinuity,and chaotic/hummock-like reflections.All above-mentioned descriptions are diagnostic of beach bar deposits.By combining diagnostic sedimentary structures and grain-size distribution pat-terns,we subdivided the system into alongshore,nearshore,and storm-influenced offshore beach bars.In addition,we found that material sources were derived mainly from wave-reworked and far-traveled sands of the braided-delta front in the Weizhou Oilfield to the north,and supplemented by basement-derived detritus from the Weixin-an low uplift.During deposition time,the Hai-3 and Hai-4 structures formed subaqueous low-relief highs.Al-though Fault#3 separated the north-south depositional realm,cross-fault sediment supply persisted,in which low uplifts became sand accumulation sites.Meanwhile,joint paleodepth inversion based on paleontology,wave-ripple parameters,and facies-thickness stacking indicated that alongshore beach bars were formed at~0-3 m wa-ter depth,nearshore beach bars at~3-8 m,and offshore beach bars at~8-11 m.Therefore,we proposed a"source-paleo-uplift-paleodepth"co-control model for beach bar deposition,provided a basis for beach bar-type reservoir identification,key-controller identification,and horizontal prediction in the Haizhong Sag,and pro-moted the applicability to similar lacustrine rift basins.

张尚虎

中国石化上海海洋油气分公司,上海 200120

海洋科学

滩坝沉积规律涠洲组海中凹陷北部湾盆地

beach-barsedimentation patternWeizhou FormationHaizhong SagBeibuwan Basin

《海洋地质前沿》 2026 (3)

53-63,11

中国石化集团公司科技项目(P25121,P23245)

10.16028/j.1009-2722.2025.190

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