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    薄互层滩坝砂体的定量预测——以东营凹陷古近系沙四上亚段(Es上4)为例

    The quantitative prognosis of thin interbedded beach-bar sandbodies: a case study of the upper 4th submember of the Paleogene Shahejie Formation in Dongying Sag

    • 摘要: 提要:薄互层砂体的定量预测是沉积学研究的难点之一。滩坝是滨浅湖区典型的薄互层砂体,其预测和勘探难度大。通过对东营凹陷古近系沙四上亚段滩坝的沉积特征、平面分布及控制因素等研究,认为滩坝的形成与分布主要受不同波浪带控制,即冲浪回流带控制沿岸滩坝(包括砾质滩坝)、碎浪带控制近岸滩坝、破浪带控制远岸滩坝。在建立了东营凹陷风动力砂体分布模型基础上,通过分析不同波浪带波浪参数变化,建立了破浪带和碎浪带砂体定量预测模型,对东营凹陷博兴洼陷南部缓坡带近岸坝、远岸坝单砂体的厚度及宽度进行了定量预测计算,并对砂体的延伸长度通过微地貌恢复+风动力技术结合进行了计算。然后通过统计单个坝砂体厚度和连井对比对预测砂体厚度、宽度及长度进行了检验验证,二者吻合较好,证明预测方法切实可行。最后认为,6~8级风力最有利于滩坝的形成。该方法为薄互层砂体的定量预测研究提供了一种新的分析思路,对隐蔽油藏勘探有指导作用,但该方法不适用于明显受物源控制薄砂体的预测。

       

      Abstract: Abstract:The quantitative prognosis of thin interbedded sandbodies is one of the difficulties in sedimentological research. The beach-bar is a typically thin interbedded sand body in shore-shallow lake whose prediction and exploration are very difficult. Based on the study of sedimentary characteristics, plane distribution and controlling factors of beach-bar in the upper 4th submember of the Paleogene Shahejie Formation in Dongying Sag, the authors consider that the development and distribution of beach-bar are mainly controlled by different wave zones, i.e., the surfing-backflowing zone controls pebble beach-bar and longshore beach-bar, the breaker zone controls nearshore beach-bar and the broken zone controls infralittoral shore beach-bar. Based on the wind-dynamic sandbodies distribution model and the analysis of wave parametric variation in different zones, the authors established the quantitative prognostic models of the sand body in the broken zone and the breaker zone, and calculated the thickness and width of sandy bar distribution in nearshore and infralittoral shore. In addition, using wind-dynamic mixed microtopography recovering technique, the authors obtained the extension length of the sandy. By employing statistics of single layer bar thickness and well connecting correlation, the authors examined the predicted results and proved them to be reliable and reasonable. It is demonstrated that the 6-8 wind scale is favorable for the development of the beach-bar. This method provides a new insight for the prediction of thin sand body and is useful to the exploration of subtle reservoirs; nevertheless, it is not suitable for the prediction of the thin sand body mainly controlled by the provenance.

       

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