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Stochastic simulations of dependent geological variables in sandstone reservoirs of Neogene age: A case study of Kloštar Field, Sava Depression

机译:新近纪时代砂岩储层相关地质变量的随机模拟:以萨瓦ava陷克洛什塔尔油田为例

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摘要

The research presented herein is the first attempt to perform geostatistical simulations on three geologic variables, porosity, thickness, and depth to reservoir, in the Croatian Pannonian basin. The data were collected from a reservoir of Lower Pontian age in Kloštar Field, located in the western part of the Sava Depression.All three variables were analyzed using sequential Gaussian simulations (SGS). Information regarding present-day depth, thickness, and locations of areas with higher porosity values were used to reconstruct paleo-depositional environments and the distribution of different lithotypes, ranging from medium-grained, to mostly clean sandstones and to pure, basin marls. Estimates of present-day thickness and depth can help to define areas of gross tectonic displacement and the role of major faults that have been mapped in the field. However, since mapping of the raw data (including porosities) does not allow the reconstruction of paleo-depositional environments, sequential indicator simulations (SIS) were applied as a secondary analytical tool. For this purpose, several cutoff values for thickness were defined in an effort to distinguish the orientation of depositional channels (main and transitional). This was accomplished by transforming porosities to indicator values (0 and 1) and by applying a non-linear “indicator kriging” technique as the “zero” map for obtaining numerous indicator realizations by SIS.In the SGS and the SIS approaches, the simulations encompassed 100 realizations. A representative realization was then selected using purely statistical criteria, i.e., two realizations were almost always chosen in accordance with the order of calculation. The 1st and 100th realizations were selected for each variable in the SGS and SIS and five “indicator kriging” maps were chosen for the thicknesses cutoffs.
机译:本文介绍的研究是对克罗地亚Pannonian盆地中的三个地质变量(孔隙度,厚度和储层深度)进行地统计学模拟的首次尝试。这些数据是从位于萨瓦pression陷西部的克洛什塔尔油田下笨珍时代的一个储层中收集的,所有三个变量都使用顺序高斯模拟(SGS)进行了分析。使用有关当今深度,厚度和孔隙率较高区域的位置的信息来重建古沉积环境和不同岩石类型的分布,范围从中粒到大部分为干净的砂岩,再到纯净的盆地泥灰岩。对当今厚度和深度的估计可以帮助确定总体构造位移的区域以及在现场测绘的主要断层的作用。但是,由于原始数据的映射(包括孔隙度)不允许重建古沉积环境,因此采用了顺序指示器模拟(SIS)作为辅助分析工具。为此,定义了几个厚度截止值,以区分沉积通道(主通道和过渡通道)的方向。这是通过将孔隙率转换为指标值(0和1)并应用非线性“指标克里金法”技术作为“零”图来获得SIS实现的众多指标实现的。在SGS和SIS方法中,模拟包含100个实现。然后使用纯粹的统计标准选择一个有代表性的实现,即几乎总是根据计算顺序选择两个实现。为SGS和SIS中的每个变量选择了第一个和第100个实现,并为厚度截止选择了五个“指示器克里金”图。

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