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首页> 外文期刊>Journal of Petroleum Exploration and Production Technology >Integrated 3D facies modeling of the Mangahewa Formation, Maui Gas Field, Taranaki Basin, New Zealand
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Integrated 3D facies modeling of the Mangahewa Formation, Maui Gas Field, Taranaki Basin, New Zealand

机译:新西兰塔拉纳基盆地毛伊气田Mangahewa组的集成3D相建模

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摘要

3D seismic data, well logs, core-based lithofacies and photographs have been combined to interpret and model the depositional facies of the Mangahewa Formation of the Maui Gas Field, Taranaki Basin, New Zealand. The primary objective of the study is to generate a robust facies model for the Middle to Late Eocene (47–37?Ma) Mangahewa Formation of the field. The facies model has included eighteen depositional facies spatially distributed over the gas field. These facies are further subgrouped into three broad depositional facies associations, namely marginal marine, shallow marine and offshore environment. We have identified that marginal marine is the most dominant facies association (64%) within the model. The model visualizes estuarine and shoreface sand geobodies dominating over other facies within the model. Both geobodies comprise over 40% of all the facies interpreted in the field. The entire modeling process involves a novel stochastic approach using unique workflow that follows 3D gridding, coding of the facies classes and multiple iterations over the interpreted facies. The model therefore realistically visualizes potential facies responsible for “good”-quality reservoir sands in the Mangahewa Formation with possible retrogradation from older to younger succession.
机译:结合了3D地震数据,测井,基于岩心的岩相和照片,以解释和模拟新西兰塔拉纳基盆地毛伊气田的Mangahewa组的沉积相。该研究的主要目的是为该油田的中至始新世(47-37?Ma)Mangahewa组生成一个可靠的相模型。相模型包括在气田上空间分布的十八个沉积相。这些相被进一步细分为三个广泛的沉积相协会,即边缘海洋,浅海和近海环境。我们已经确定边缘海相是该模型中最主要的相相(64%)。该模型将主导模型中其他相的河口和滨海砂土体形象化。两种地质体占该领域解释的所有相的40%以上。整个建模过程涉及一种新颖的随机方法,该方法使用独特的工作流程,该工作流程遵循3D网格化,相类编码和对解释后相的多次迭代。因此,该模型现实地可视化了Mangahewa组中“优质”优质储层砂岩的潜在相,并可能从较旧的演替阶段向较年轻的演替阶段回退。

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