首页|渤海湾盆地渤中凹陷烃源岩形成与演化的主控因素

渤海湾盆地渤中凹陷烃源岩形成与演化的主控因素

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渤海油田是目前中国第一大油田,渤中凹陷是渤海海域油气最富集的生烃凹陷.综合应用地震、钻井和测试分析,评价渤中凹陷烃源岩品质及其在平面和纵向分布的差异性.从断裂、物源及地层热沉降等地质方面,分析烃源岩形成与演化的主控因素,阐述了渤中凹陷是最富烃凹陷的原因.结果表明,渤中凹陷古近系沙河街组三段(沙三段)、沙河街组一段(沙一段)和东营组三段(东三段)烃源岩总有机碳平均值分别为2.06%,1.95%,1.59%;沙三段、沙一段、东三段有机质类型分别以Ⅱ1型、Ⅰ-Ⅱ1型和Ⅱ1-Ⅱ2型干酪根为主.沙三段和沙一段烃源岩已达到高成熟-过成熟阶段,东三段烃源岩大面积属于高成熟阶段.断层的规模和活动强度控制了烃源岩的形成与分布,渤中凹陷各次洼烃源岩分布具有差异性.渤中凹陷位于渤海湾盆地中心,远离盆外物源,中渐新世以前以盆内小物源为主,欠补偿沉积时间较长,半深湖-深湖相面积大,决定了渤中凹陷烃源岩层系最多且厚度最大.渤中凹陷在新近纪沉降幅度最大,沉积厚度最大,古近系烃源岩埋藏深、演化程度高,生成的油气最富集.研究成果可为渤中凹陷下一步油气勘探提供依据,也可为其他相似凹陷的评价提供借鉴.
Main controlling factors for the formation and evolution of hydrocarbon source rocks in the Bozhong depression,Bohai Bay Basin
The Bohai oil field is currently China's largest oil field.The Bozhong depression is the most abundant hydrocarbon-generating depression in Bohai Sea.Based on seismic,drilling,and analytical data,the quality of source rocks and their differences in the planar and vertical distributions in the Bozhong depression are evaluated in this work.The main controlling factors for the formation and evolution of source rocks are analyzed from geological aspects such as faults,provenance,and thermal subsidence of the strata,providing natural explanations for why the Bozhong depression is the most hydrocarbon-rich depression.The results show that the average total organic carbon values of the Third member of the Shahejie Formation(Es3),the First member of the Shahejie Formation(Es1),and the Third member of the Dongying Formation(Ed3)are 2.06%,1.95%,and 1.59%,respectively,and the organic matter types of Es3,Es1,and Ed3 are mainly type Ⅱ1,type Ⅰ-Ⅱ 1,and type Ⅱ 1-Ⅱ 2 kerogens,respectively.The source rocks of Es3 and Esy are in a high overmaturity stage,while the source rocks of Ed3 are extensively in a stage of high maturity.The scale and activity intensity of faults control the formation and distribution of the source rocks,resulting in the different distributions of the source rocks in various parts of the Bozhong depression.Located in the center of Bohai Bay Basin,the Bozhong depression is far away from external provenance.Before the middle Oligocene epoch,small scale provenances were widely distributed within the basin.Long-term uncompensated sedimentation has contributed to the area an increase of semi-deep and deep lake facies,in which the sources rocks of the Bozhong depression formed in multiple layers with high thickness.Due to the large subsidence range and sedimentary thickness that occurred during the Neogene period,as well as the deep burial depth and high evolution degree of hydrocarbon source rocks deposited during the Paleogene period,the oil and gas in the Bozhong depression are more enriched compared to other depressions in Bohai Bay Basin.The results of this study not only provide a good basis for further hydrocarbon exploration in the Bozhong depression,but also supply a reference for the evaluation of other similar depressions.

source rockfault activityprovenance supplysettling velocityBozhong depression

张莹、刘志峰、陈少平、贾万丽、雷杭山

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中海油研究总院有限责任公司,北京 100028

烃源岩 断裂活动 物源供给 沉降速度 渤中凹陷

2024

成都理工大学学报(自然科学版)
成都理工大学

成都理工大学学报(自然科学版)

CSTPCD北大核心
影响因子:1.596
ISSN:1671-9727
年,卷(期):2024.51(6)