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Chemostratigraphy of the Upper Cretaceous from Central and South Texas with focus on the Eagle Ford group.

机译:得克萨斯州中部和南部得克萨斯州上白垩统的化学地层学,重点是鹰福特集团。

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摘要

The fine-grained organic-rich rocks of the Eagle Ford (Cenomanian-Turonian) were deposited during the Upper Cretaceous in the shallow waters of the Western Interior Seaway. Five drill cores recovered from two counties, four from Travis County, Texas and one from Frio County, Texas, have been scanned from between two foot and half foot intervals with a hand-held energy-dispersive x-ray fluorescence (HH-ED-XRF) spectrometer to acquire major (e.g. Ca, Si, Al) and trace (e.g. Mo, V, Ni) element data for quantitative analysis. Additionally, gamma ray logs have been analyzed for two of the cores.;Major element geochemistry indicates the Eagle Ford deposited in South Texas is different from the Eagle Ford deposited in Central Texas. South Texas Eagle Ford is much more Ca (carbonate) rich, with a noticeably lower Al (clay) content. South Texas and Central Texas Eagle Ford both have low Si (quartz) content relative to the Al and Ca content, indicating a negligible siliciclastic contribution during deposition. Trace element analysis reveals the redox conditions of the bottom waters during deposition. Mn---an element which becomes mobile and may be removed from an open system in reducing conditions---levels are much higher in the Austin Chalk and Buda with notably lower values in the Eagle Ford in both Central Texas and South Texas. Mo, an element which tends to bind with organic matter or sulfides during reducing conditions, is notably higher in the Eagle Ford of both South Texas and Central Texas. The correlation of decreased Mn levels and increased Mo levels suggests that the Eagle Ford was deposited in reducing conditions in an open system capable of removing mobilized Mn.;Geochemical analysis of major and trace elements obtained from ED-XRF may be used in the petroleum industry in concert with XRD, electric logs, and standard core analysis to give a more complete picture of the depositional environment, clay type and volume, geophysical rock properties, and areal extent of a potential unconventional shale reservoir for hydrocarbon extraction. XRF data offers insight about the rocks, leading to improved understanding of the depositional environment and chemical makeup. Applying these technologies to the Eagle Ford helps unlock the potential of this significant hydrocarbon source and reservoir.
机译:Eagle Ford(Cenomanian-Turonian)的细颗粒富含有机物的岩石在上白垩统时期沉积在西部内海道的浅水中。已使用手持式能量分散X射线荧光仪(HH-ED- XRF光谱仪可获取主要(例如Ca,Si,Al)和痕量(例如Mo,V,Ni)元素数据以进行定量分析。此外,还对其中两个岩心进行了伽马射线测井分析。主要元素地球化学表明,沉积在南德克萨斯州的Eagle Ford与沉积在德克萨斯中部的Eagle Ford不同。南得克萨斯州的伊格福特更富Ca(碳酸盐),而Al(粘土)的含量明显较低。相对于Al和Ca含量,南得克萨斯州中部和得克萨斯州中部的伊格福特都具有较低的Si(石英)含量,这表明沉积过程中硅质碎屑的贡献可忽略不计。微量元素分析揭示了沉积过程中底水的氧化还原条件。 Mn-一种可移动的元素,可以在开放条件下从开放系统中除去-在Austin Chalk和Buda中含量高得多,在Texas Texas和South Texas中Eagle Ford中的含量特别低。钼是一种在还原条件下易于与有机物或硫化物结合的元素,在南德克萨斯州和德克萨斯州中部的伊格福特地区尤其明显。锰含量降低和钼含量升高之间的相关性表明,Eagle Ford在还原条件下以能够去除动员的锰的开放系统沉积。与XRD,电测井和标准岩心分析相结合,可以更完整地了解沉积环境,黏土类型和体积,地球物理岩石特性以及潜在的非常规页岩油藏的面积范围,以进行烃类开采。 XRF数据提供了有关岩石的见识,从而使人们对沉积环境和化学成分有了更深入的了解。将这些技术应用到Eagle Ford有助于释放这种重要的烃源和储层的潜力。

著录项

  • 作者

    Huffman, Brett.;

  • 作者单位

    The University of Texas at Arlington.;

  • 授予单位 The University of Texas at Arlington.;
  • 学科 Geology.
  • 学位 M.S.
  • 年度 2013
  • 页码 82 p.
  • 总页数 82
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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