首页> 外文期刊>Marine and Petroleum Geology >Facies and porosity 3D models constrained by stochastic seismic inversion to delineate Paleocene fluvial/lacustrine reservoirs in Melut Rift Basin, Sudan
【24h】

Facies and porosity 3D models constrained by stochastic seismic inversion to delineate Paleocene fluvial/lacustrine reservoirs in Melut Rift Basin, Sudan

机译:由随机地震反演的面部和孔隙率3D模型在苏丹金属裂解盆地描绘古典型河流/湖湖水储层

获取原文
获取原文并翻译 | 示例
           

摘要

The Paleocene sandstones of the Yabus and Samma formations are the main oil reservoirs in the Melut Rift Basin of interior Sudan. In our study area, we implemented a multi-modeling approach to reveal heterogeneity and reservoir characteristics of this sandstone. It estimates acoustic impedance from seismic data using deterministic and stochastic inversion algorithms. We integrated petrophysical and geostatistical analyses of the well logs to produce facies and porosity 3D models. The study populated and evaluated three different porosity models; one from well logs only, a second from well logs constrained by inversion results, and a third from well logs constrained by inversion results and facies. Stochastic inversion reveals a significant vertical facies heterogeneity as less as two meters in Yabus Sandstone. This heterogeneity is a lithology dependent and facies distribution is structurally controlled by major faults that developed during the third rift phase. The geostatistical integration of seismic inversion, sedimentologic and stratigraphic analyses reveal lateral facies distribution in the study area. The significant correlation between facies distribution and porosity allows reliable mapping of thin sandbodies. The facies and porosity 3D models indicate vertically-stacked channels with isolated sandbodies in Yabus Sandstone. This strongly suggests a meandering origin for this sandstone. However, the thick sandbodies observed in Samma Formation might indicate a braided channel setting. The dominant claystone and mudstone facies deposited in Melut Formation indicate a shallow lacustrine setting. The reservoir quality decreases with depth from the Paleocene Yabus and Samma formations at the top towards the Cretaceous Melut Formation at the bottom. The porosity estimates support this conclusion as detected low porosity (as less as 5%) in Melut Formation with respect to higher porosity (as high as 25%) in Yabus and Samma formations. The fades and porosity 3D models enhanced our understanding in predicting the reservoir heterogeneity, quality and architecture of this sandstone.
机译:Yabus和Samma地层的古代砂岩是室内苏丹金属裂缝盆地的主要石油储层。在我们的研究领域,我们实施了一种多模型方法来揭示这种砂岩的异质性和储层特征。它使用确定性和随机反转算法估计来自地震数据的声阻抗。我们综合了井原木的岩石物理和地统计分析,以产生面部和孔隙度3D模型。该研究填充并评估了三种不同的孔隙型模型;仅从井日志中,一秒从井日志受到反演结果的约束,以及由反演结果和相位受到的井日志中的第三个。随机反转显示出显着的垂直面,异质性,尤布斯砂岩中的两米。这种异质性是依赖性的,并且相片分布在结构上通过在第三裂阶段开发的主要故障来控制。地震反演,沉积和地层分析的地统计整合揭示了研究区的侧面分布。相分布与孔隙率之间的显着相关性允许可靠的薄砂纤维映射。面部和孔隙度3D模型表示雅布砂岩中垂直堆叠的频道,含有孤立的砂岩。这强烈建议这种砂岩的蜿蜒起源。然而,在Samma形成中观察到的厚砂囊可能表示编织渠道设置。沉积在丝瓜形成中的主要粘土和泥岩相表明浅层落叶树。储层质量随着深度从距离距离距离谷族Yabus和Samma形成的深度而降低。孔隙率估计在玉米和萨姆玛地层中的孔隙率(高达25%)中检测到晶体形成中的低孔隙率(低至5%)。淡化和孔隙度3D模型提高了我们在预测该砂岩的水库异质性,质量和结构方面的理解。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号