源内不同微相砂岩储层差异及对开发效果的影响—以庆城油田长71-2亚段为例
- 收稿日期:
2024-12-30
- 网络出版日期:
2025-09-04
摘要: 庆城油田延长组长71-2亚段致密砂岩夹层为典型的湖底扇沉积,但对沉积微相尺度上砂岩储集性能差异研究不足,制约了高产区块筛选和水平井生产效果差异分析。基于岩心、测井及地震资料,利用薄片鉴定、扫描电镜、微米CT、核磁共振、高压压汞及恒速压汞等试验,并结合试油试采数据,剖析不同沉积微相致密砂岩岩矿、微观孔隙结构、含油性和可动性、试油等方面存在的差异。结果表明:受多级坡折带控制,多期湖底扇砂体在相对平缓的半深湖-深湖坡脚带堆积,与富有机质泥页岩频繁间互,形成了大面积“三明治”源储共生,构成了庆城油田夹层型页岩油主要地质甜点,其中砂岩夹层可划分为水道、朵叶主体、朵叶侧缘、滑塌体4种沉积微相,水道、朵叶主体、朵叶侧缘砂岩叠置厚度相对较大,测井解释普遍为油层,是水平井开发的主要靶体;水道、朵叶主体、朵叶侧缘储集空间均以溶蚀孔和粒间孔为主,胶结物主要为铁白云石、铁方解石和石英,水道和朵叶主体具有填隙物和胶结物含量低、面孔率高、物性及微观孔隙结构好的特征,连通孔隙体积占比高,孔喉半径尺寸大,具有相对较高的可动流体饱和度和含油性;可动流体饱和度与孔隙结构密切相关,受微观孔隙结构控制,水道相比朵叶主体具有更好的微观孔喉参数,更有利于油气的充注和渗流;在同等厚度规模下,水道相比朵叶主体直井试油更容易获得高产工业油流,水道和朵叶主体纵向叠置是高产的沉积组合箱体;精细湖底扇致密砂岩沉积微相刻画,优化水平井方位和长度,优选有利的微相组合进行开发是提高水平井油层钻遇率和开发效果的关键。
The difference of sandstone reservoirs with different microfacies in the source and its influence on the development effect -Taking the Chang 71-2 sub-member of Qingcheng Oilfield as an example
- Received Date:
2024-12-30
- Available Online:
2025-09-04
Abstract: The tight sandstone interlayer of the Chang 71-2 sub-member of the Yanchang Formation in the Qingcheng Oilfield is a typical sublacustrine fan deposit. However, the research on the difference of sandstone reservoir performance on the sedimentary microfacies scale is insufficient, which restricts the screening of high-yield blocks and the difference analysis of horizontal well production effects. Based on core, logging and seismic data, using thin section identification, scanning electron microscopy, micro-CT, nuclear magnetic resonance, high-pressure mercury injection and constant-rate mercury injection tests, combined with oil test and production test data, the differences in tight sandstone rock and ore, microscopic pore structure, oil content and mobility, and oil test in different sedimentary microfacies are analyzed. The results show that under the control of multi-stage slope break zones, multi-stage sublacustrine fan sand bodies accumulate in the relatively gentle semi-deep lake-deep lake slope toe zone, and frequently interact with organic-rich shale to form a large area of ' sandwich ' source-reservoir symbiosis, which constitutes the main geological dessert of interlayer shale oil in Qingcheng Oilfield. The sandstone interlayer can be divided into four sedimentary microfacies : channel, lobe, lobe side edge and slump body. The sandstone superimposed thickness of channel, lobe and lobe side edge is relatively large, and the logging interpretation is generally oil layer, which is the main target of horizontal well development. The reservoir space of channel, lobe body and lobe lateral margin is dominated by dissolution pores and intergranular pores. The cements are mainly ferrodolomite, ferrocalcite and quartz. The channel and lobe body have the characteristics of low content of interstitial materials and cements, high surface porosity, good physical properties and microscopic pore structure, high proportion of connected pore volume, large pore throat radius, and relatively high movable fluid saturation and oiliness. The saturation of movable fluid is closely related to the pore structure. Controlled by the microscopic pore structure, the channel has better microscopic pore throat parameters than the lobe, which is more conducive to the filling and seepage of oil and gas. Under the same thickness scale, the channel is easier to obtain high-yield industrial oil flow than the lobed body vertical well test, and the vertical superposition of the channel and the lobed body is a high-yield sedimentary combination box ; fine sublacustrine fan tight sandstone sedimentary microfacies characterization, optimizing the orientation and length of horizontal wells, and optimizing favorable microfacies combinations for development are the key to improving the drilling rate and development effect of horizontal well reservoirs.