日本地球惑星科学連合2018年大会

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[JJ] 口頭発表

セッション記号 S (固体地球科学) » S-CG 固体地球科学複合領域・一般

[S-CG66] 3次元地質モデリングとシミュレーションの新展開

2018年5月22日(火) 10:45 〜 12:15 A10 (東京ベイ幕張ホール)

コンビーナ:高野 修(石油資源開発株式会社技術研究所)、木村 克己(独立行政法人防災科学技術研究所)、座長:木村 克己(防災科学技術研究所)

11:30 〜 11:45

[SCG66-03] 石油ポテンシャル評価のための三次元地質・堆積相モデリングワークフロー:仁賀保亜堆積盆女川層モデリングの例

*高野 修1熊田 祐子2 (1.石油資源開発株式会社技術研究所、2.三井石油開発)

キーワード:モデリングワークフロー、仁賀保亜堆積盆、地球統計学シミュレーション

This paper presents principal workflow of three-dimensional (3D) geologic and facies modeling for the purpose of petroleum potential evaluation. Because the petroleum system factors are so complex, the modeling procedure tends to be various depending on the modeling purpose and geologic settings. This case study adopts the structural geological, sedimentological, sequence stratigraphical and geostatistical methods in the modeling to obtain precise results on the reservoir facies distributions, connectivity and volumetrics. The example modeling target is the Onnagawa Formation, which mainly consists of hybrid source and reservoir rock-type siliceous shale, distributed in the Nikaho subbasin of the Akita basin, northeast Japan. The major data sources are from exploration well and 2D/3D seismic survey data sets. This study conducted modeling mainly utilizing software on a workstation.

The first step starts with the 3D structural modeling using major stratigraphic surfaces, such as formation boundaries, which are derived from seismic horizons and well stratigraphic marker data. All these source data are interpolated and extrapolated to create a 3D horizon surface. In case 3D seismic survey data exists, horizon picking automatically leads to horizon surface creation.

The second step focuses on facies determination on the well logs (log facies) and seismic sections (seismic facies) to associate the rock property type with sedimentological framework. If needed, facies association, which is a group of associated facies, can be determined. In the case of the Nikaho subbasin, three facies associations were recognized. All the divided facies information is plotted on a map to create conceptual depositional model.

The third step conducts sequence stratigraphic division to create sedimentologically meaningful finer layers, by which basic modeling layers are created and detailed depositional system/facies distribution maps are created. In the case of the Nikaho subbasin, four depositional sequences were recognized in the Onnagawa Formation. The depositional process as a controlling factor of facies distributions is also discussed at this step.

The fourth step is the geostatistical integration of well-log petrophysics data and seismic attributes to determine reservoir properties of each facies class.

In the final step, geostatistical facies modeling is conducted for each depositional sequence unit. At this step, facies are distributed using stochastic simulation methods with well data as hard data and seismic attributes as soft data. Stochastic simulation method can be selected depending on the data condition and ultimate purpose of the modeling. In the case of the Nikaho subbasin, sequential indicator simulation was selected for facies distribution simulation. Depositional trend in accordance with the estimated depositional systems and processes was also given as soft data to control facies distributions.