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Petrophysical rock typing of unconventional shale plays: A case study for the Niobrara Formation of the Denver-Julesburg (DJ) Basin.

机译:非常规页岩气的岩石物理岩石分型:以丹佛-朱尔斯堡(DJ)盆地的尼奥布拉拉组为例。

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摘要

A petrophysical rock typing has been performed based on a methodology that integrated depositional and petrophysical rock analysis to identify distinct rock types in the Niobrara Formation of the Denver-Julesburg (DJ) Basin. The depositional rock analysis incorporated a literature study, interpretations of the geologic depositional setting and sequence stratigraphy, core descriptions, and analysis of well-log data. The petrophysical rock analysis was carried out using experimental core data on mineralogy, pore characterization, source rock evaluation, micro-textural image analysis, and ultrasonic acoustic velocity and anisotropy interpretations.;Six Niobrara Formation lithofacies and three similar lithofacies-groups (All Marls, Middle Chalks, and Basal Chalk) were identied in the target well interval through the depositional rock analysis within the context of the large-scale geologic framework. The pore-scale petrophysical rock analysis was carried out to investigate whether these lithofacies-groups followed distinct rock types in the Niobrara Formation based on the analysis of experimental core data.;The conclusions reached in this study included that, based on the mineralogy, pore structure, and acoustic velocity interpretations, the Basal "Chalk" may be a Basal Marl - at least locally in the studied target well. However, the Basal Chalk rocks contain lowest source rock potential and are not likely to contribute to economic hydrocarbon production for the target well. Both the All Marls and the Basal Chalk rock-groups have higher porosity, smaller pores, and smaller pore throats than the Middle Chalks. The rocks in the Middle Chalks have higher stiffness and pressure compliant pores.;The Niobrara Formation is an unconventional petroleum system - its hydrocarbon-rich mudrock units were deposited in a shallow marine environment and have evolved as oil- and gas-prone source and reservoir rocks. Significant pore-scale variability in mineralogy, pore characterization, organic matter distribution, and acoustic velocity and anisotropy properties exist in these rocks. Hydrocarbon production from its low-porosity, nanodarcy permeability, and interbedded chalk-marl reservoir interval is very challenging.;The petrophysical rock typing methodology adopted in this case study can be a useful formation evaluation tool for the Niobrara Formation. It can provide valuable information about its rock matrix, such as, the lithofacies identification and descriptions through depositional rock analysis, identifying reservoir and sourcing intervals, mineralogy analysis, organic matter evaluation, pore characterization, and acoustic velocity and anisotropy properties.
机译:已经基于一种方法对岩石物性进行了分型,该方法将沉积和岩石物性分析相结合,以识别丹佛-尤尔斯堡(DJ)盆地Niobrara组中不同的岩石类型。沉积岩分析结合了文献研究,地质沉积环境和层序地层学解释,岩心描述以及测井资料分析。岩石物理分析是利用矿物学,孔隙特征,烃源岩评估,微观纹理图像分析以及超声声速和各向异性解释的实验核心数据进行的;六个Niobrara组岩相和三个类似岩相组(All Marls,在大型地质框架下,通过沉积岩分析,在目标井段内确定了中粉笔和基粉笔。通过对实验岩心数据的分析,进行了孔隙尺度的岩石物性分析,以研究这些岩相在Niobrara组中是否遵循不同的岩石类型;这项研究得出的结论包括基于矿物学的孔隙在结构和声速的解释上,基底“粉笔”可能是基底马尔,至少在研究目标井中是局部的。但是,基础粉笔岩含最低的烃源岩潜力,不太可能有助于目标井的经济油气生产。与中白垩岩相比,All Marls和基底白垩岩组均具有较高的孔隙度,较小的孔隙和较小的孔喉。中白垩岩中的岩石具有较高的刚度和压力顺应性孔隙。Niobrara地层是非常规的石油系统-其富含烃的泥岩单元沉积在浅海环境中,并演变成易生油气的储层岩石。这些岩石中存在矿物学,孔隙特征,有机质分布以及声速和各向异性等方面的显着孔隙尺度变化。低孔隙度,纳达斯渗透率和层状白垩-大理石储集层间的油气成藏非常具有挑战性。该案例研究采用的岩石物理岩石分型方法可作为Niobrara地层的有用评价工具。它可以提供有关其岩石基质的有价值的信息,例如,通过沉积岩石分析,识别储层和采出层段,矿物学分析,有机质评估,孔隙表征以及声速和各向异性特性,进行岩相识别和描述。

著录项

  • 作者

    Kamruzzaman, Asm.;

  • 作者单位

    Colorado School of Mines.;

  • 授予单位 Colorado School of Mines.;
  • 学科 Petroleum geology.;Petrology.;Mineralogy.
  • 学位 M.S.
  • 年度 2015
  • 页码 96 p.
  • 总页数 96
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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