古地貌对湖盆相特征及储层预测的影响——以中国SL盆地西斜坡白垩系储层为例

Longtao Cui, Qianping Zhang, Xue Liu, Ming Yang, Jianmin Zhu
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引用次数: 0

摘要

中国SL盆地西斜坡主要面向岩性油气藏。古地貌和物源方向分析对预测砂体类型和分布具有重要意义。根据测井、岩心和地震资料分析,研究区主要发育辫状三角洲和重力沉积。采用回跳法重建了白垩纪青山口至姚家组的地形。西坡主要受青山口组两条斜坡带控制,上坡宽度12 ~ 18 km,坡度0.7 ~ 0.8度,下坡宽度13 ~ 15 km,坡度1.0度。西坡为姚家组单坡带控制,下坡宽13 ~ 16 km,坡度0.4度。分析了斜坡带、物源方向与砂体分布的关系,结果表明,上下斜坡组合控制了储层类型的分布,物源供给速率控制了砂体的规模。当物源方向与斜坡方向平行时,重力流发育,斜坡在垂直于物源方向上成为输送通道。古地貌、湖泊水位和物源方向是西坡砂体形成的主要控制因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Paleogeomorphic Influence on Facies Characteristics and Reservoir Prediction in Lacustrine Basin—By Taking Cretaceous Reservoirs in the Western Slope of SL Basin, China as an Example
The West Slope of SL Basin, China, mainly targets on lithologic reservoirs for oil and gas. The paleogeomorphology and provenance direction analysis has great significance for predicting the type and distribution of sand body. According to the analysis of well logging, core and seismic data, braided delta and gravity sediment mainly develop in the study area. A backs tripping method is used to reconstruct the topography of Qingshankou to Yaojia Formation, Cretaceous. The West Slope is mainly controlled by two slope belts in Qingshankou Formation, with the width of upper slope 12 - 18 km and the gradient 0.7 - 0.8 degrees, the width of lower slope 13 - 15 km and the gradient 1.0 degrees. The West Slope is controlled by a single slope belt in Yaojia Formation, with the lower slope width of 13 - 16 km and the gradient 0.4 degrees. The relationship between the slope belt, provenance direction and sand body distribution is analyzed, and result shows that the combination of upper and lower slope controls the distribution of reservoir types, and the provenance supply rate controls the scale of sand body. The gravity flow develops when the provenance direction is parallel to slope direction, and the slope becomes transporting channel in vertical to provenance direction. The paleogeomorphology, lake level and provenance direction are the main control factors of sand body in West Slope.
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