首页|基于地震沉积学和沉积物理模拟的河流决口扇沉积演化过程分析——以渤海K油田明化镇组下段为例

基于地震沉积学和沉积物理模拟的河流决口扇沉积演化过程分析——以渤海K油田明化镇组下段为例

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为厘清渤海海域K油田明化镇组下段砂体分布特征,为下一步的目标优选提供参考依据,基于优选的地层属性地震切片和测井响应特征,分析了明化镇组下段沉积演化过程,设计了沉积物理模拟对比实验.结果表明:①平均负振幅属性最能反映该地区沉积特征且该属性特征与测井曲线特征结合最好,确立5种地震属性相分别对应于强水动力下的决口扇沉积、弱水动力下的决口扇沉积、曲流河沉积、分支河道沉积、洪漫沉积;②渤海K油田主要发育河流决口扇沉积,分为前期的洪漫沉积与决口扇沉积、中期的扇上下切河道沉积及分支河道沉积、末期的曲流河道沉积3个部分,平面差异分布较为明显;③沉积模拟实验共分为洼地填充期、扇体改造期、支流发育期、汇聚摆动期,与渤海K油田明化镇组下段沉积演化有较好的对应,很好地验证并再现了河流决口体系演化过程.以上认识明确了明下段在K油田地区的沉积演化特征,有利于该地区的勘探评价,物理模拟验证也提供了 一种新的研究思路.
Analysis of the sedimentary evolution process of crevasse splay based on seismic sedimentology and sedimentary physics simulation:An example from the lower section of Minghuazhen Formation of K oilfield in Bohai sea
To clarify the distribution characteristics of sand bodies in the lower section of the Minghuazhen Formation of K oilfield in Bohai sea and to provide a reference basis for the next target selection,seismic slices of stratum attribute were selected and combined with logging characteristics to establish the seismic attribute faces.Additionally,the sedimentary evolution process of this section was analyzed,and a comparative sedimentary physics experiment was designed to verify the results.The results of the study are as follows:①The average negative amplitude best reflects the deposit characteristics of the area and this attribute is best integrated with the logging curve characteristics.Five seismic attribute faces are established and correspond to strong hydrodynamic crevasse-splay deposit,weak hydrodynamic crevasse-splay deposit,meandering river deposit,distributary channel deposit,and floodplain deposit.②The K oilfield in Bohai sea mainly develops crevasse splay deposits,which are divided into three parts,namely floodplain deposits and crevasse-splay deposits in the early stage,channel deposits of upper and down splay cuts and distributary channel deposits in the middle stage,and meandering river deposits in the later stage,with a more obvious planar difference distribution.③The physical simulation experiment is divided into depression filling,splay modification,tributary development and convergent oscillation periods,which correspond well with the sedimentary evolution of the lower section of the Minghuazhen Formation of K oilfield in Bohai sea,and well validate and reproduce the evolution of the river outfall systems.The above understandings refine the sedimentary evolution of the lower section of Minghuazhen Formation of K oilfield,which is beneficial to the exploration and evaluation of the area.And the physical simulations experiment also provides a new research method.

crevasse splaysedimentation processesBohai seaMinghuazhen Formationseismic sedimentologyphysical simulation of sedimentation

胡晓红、尹太举、任大伟

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长江大学地球科学学院 湖北武汉 430100

河流决口扇 沉积过程 渤海海域 明化镇组 地震沉积学 沉积物理模拟

国家自然科学基金国家自然科学基金重点项目

4167211942130813

2024

中国海上油气
中海石油研究中心

中国海上油气

CSTPCD北大核心
影响因子:1.266
ISSN:1673-1506
年,卷(期):2024.36(2)
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