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Structural, stratigraphic, and reservoir characteristics of natural gas production from the Boone Formation, Batson and Ozone fields, Arkoma Basin, western Arkansas.

机译:阿肯色州西部阿科玛盆地Boone组,Batson和Ozone油田天然气生产的结构,地层和储层特征。

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摘要

The Kinderhookian-Osagean Boone Formation is a fossiliferous limestone with considerable interbedded chert present across the Ozark shelf and northern Arkoma basin. The Boone Formation has produced more than 23.5 billion cubic feet of natural gas in northern Arkansas primarily from the Arkoma Basin. 68% of total Boone production is from Batson and Ozone fields.; Batson and Ozone fields have produced anomalous amounts of natural gas from the Boone Formation from two related fault/fold combination traps. These traps are present in a single east-west anticline, separated into a northern and southern trap by a central graben formed by east-west striking antithetic normal faults. A paleo-high, sub-aerial exposure, and karst processes during the post-Boone deposition unconformity are important factors in reservoir development. Production comes from a complex and highly anisotropic reservoir, where higher porosities are consistently associated with greater chert content. Core analysis suggests that porosity development in the chert is related to syn-depositional fracturing, brecciation and possible intermittent exposure.
机译:Kinderhookian-Osagean布恩岩层是一种化石石灰岩,在Ozark陆架和北部的Arkoma盆地中存在大量的层状石。布恩组已经在阿肯色州北部生产了超过235亿立方英尺的天然气,主要来自阿科玛盆地。布恩总产量的68%来自Batson和Ozone油田。 Batson和Ozone油田是通过两个相关的断层/褶皱组合圈闭从Boone层中产生异常量的天然气的。这些圈闭存在于单一的东西向背斜中,由东西走向的对立正断层形成的中央grab陷将其分为北部和南部圈闭。布恩后沉积不整合期间的古高,地下暴露和岩溶过程是储层开发的重要因素。产量来自一个复杂且高度各向异性的储层,在该储层中,较高的孔隙度始终与较高的content石含量相关。岩心分析表明,cher石中孔隙的发育与同沉积的压裂,水化和可能的间歇性暴露有关。

著录项

  • 作者

    Davis, Clayton Yarri.;

  • 作者单位

    University of Arkansas.;

  • 授予单位 University of Arkansas.;
  • 学科 Geology.
  • 学位 M.S.
  • 年度 2007
  • 页码 126 p.
  • 总页数 126
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;
  • 关键词

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