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The Basin Modeling and Evaluation of Upper Paleocene-Eocene Source Rocks in the North-Central Gulf Coast Region

机译:北部海湾海岸地区上部古植物 - 占领源岩的盆地建模与评价

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The creation of 1D models to reconstruct Louisiana's regional thermal maturation history allows for a more accurate visualization and placement of thermal maturation zones. Analysis of the thermal maturation history of a basin will provide greater insight into the type of hydrocarbon generation by depth and location. The basic elements needed to reconstruct burial and thermal maturity histories are well log picks, temperature-depth data, and geochemical data. These histories are represented by 1D models which provide predictive value to hydrocarbon exploration by generating thermal maturity maps for a given unit. Each map indicates the stage of thermal maturity for the unit by geographic location. These maps are not intended to be finely-tuned and adjusted for local sources of variation in maturation, but instead are to be treated as a broad reference for the region of study. Local unconformities, faulting, and variations in heat flow were not considered in this study, and allochthonous salt could not be accounted for by the modeling software. The resultants have shown that the ID modeling process used in this study is comparable to that of similar studies in both methodology and results. The models and maps illustrate the present-day location of the Paleocene-Eocene interval in relation to zones of thermal maturation. The maps created are based on limited amounts of geochemical data; a larger data set would be necessary to create more accurate maps.
机译:重建路易斯安那区域热成熟历史的1D模型的创建允许更准确的可视化和放置热成熟区。盆地的热成熟历史分析将通过深度和位置对烃类产生更大的洞察力。重建埋葬和热成熟度历史所需的基本元素是日志挑选,温度深度数据和地球化学数据。这些历史由1D模型表示,通过为给定单元产生热成熟度图,为碳氢化合物勘探提供预测值。每个地图都表示通过地理位置的单位热成熟度的阶段。这些地图不旨在精确调整和调整成熟的局部变化源,而是将被视为研究区域的广义参考。本研究中不考虑局部不整合,断层和热流的变化,并且通过建模软件无法计算出交盐。结果表明,本研究中使用的ID建模过程与方法和结果中的类似研究相当。模型和地图说明了与热成熟区相对于热成熟区的古代 - 何地区的本日位置。创建的地图基于有限的地球化学数据;需要更大的数据集来创建更准确的映射。

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