首页> 外文学位 >Sequence stratigraphic controls of hydrocarbon reservoir architecture-case study of late Permian (Guadalupian) Queen Formation, Means Field, Andrews County, Texas.
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Sequence stratigraphic controls of hydrocarbon reservoir architecture-case study of late Permian (Guadalupian) Queen Formation, Means Field, Andrews County, Texas.

机译:油气储层构造的层序地层控制-以得克萨斯州安德鲁斯县Means Field晚二叠世(瓜达路普)皇后组为例。

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摘要

The late Permian Queen Formation (115 m thick) is a succession of mixed clastics, carbonates and evaporites deposited in the northeastern margin of Central Basin Platform of the Permian Basin, west Texas, USA. Depositional facies, stacking patterns of cyclic facies associations and statistical correlation of rock property variations define geologic controls on reservoir rock properties. Textural, compositional, petrophysical and diagenetic variations within lithofacies exhibit systematic changes with stratigraphic position, which can be related to base level changes that were controlled by high-frequency, low-amplitude, sea level fluctuations during a greenhouse period.; Ten lithofacies record variations in clastic input, shallow marine carbonate production, and evaporate precipitation in sabhkas and salinas. Four different types of lithofacies associations define: (1) transgressive deltaic deposits; (2) upward-shallowing evaporite and carbonate tidal-flat deposits; (3) transgressive beach ridge and sand flat deposits; and (4) upward-shallowing evaporite salina-sabhka deposits. Stacking patterns of lithofacies associations define sixteen depositional cycles that can be grouped into eight cycle sets. Cycle sets in turn are grouped to define two high-frequency sequences. Sequence 1 progresses from fluvial to carbonate tidal flat cycles. Sequence 2 consists of salina-dominated upward-shoaling cycles. Lateral continuity of cycles indicates restricted sedimentation on low-accommodation inner platform areas updip of prograding highstand platform-margin carbonate buildups, and a long-term trend of accommodation decrease. The Queen Formation contains two reservoir types; (1) siliciclastic reservoirs capped by evaporites and (2) layer-cake carbonate reservoirs. Of the four reservoir zones identified, R11 in lowstand fluvial-deltaic deposits has relatively little cement and the best reservoir characters.
机译:晚二叠纪皇后组(115 m厚)是一系列沉积在美国西德克萨斯州二叠纪盆地中央盆地平台东北缘的混合碎屑,碳酸盐和蒸发岩。沉积相,循环相联系的堆积模式以及岩石性质变化的统计相关性定义了对储集岩性质的地质控制。岩相中的质地,组成,岩石物理和成岩作用随地层位置表现出系统的变化,这可能与基准水平的变化有关,而基准水平的变化是由温室内高频,低振幅,海平面的波动控制的。十个岩相记录了碎屑输入,浅层海洋碳酸盐生产以及萨布卡和盐沼蒸发降水的变化。岩相学协会分为四种不同类型:(1)海侵性三角洲沉积; (2)浅层蒸发岩和碳酸盐滩涂沉积物; (3)海侵海岭和沙滩沉积物; (4)向上浅析的蒸发盐盐岩-萨卜卡矿床。岩相关联的堆积模式定义了16个沉积周期,这些沉积周期可以分为8个周期集。循环集又被分组以定义两个高频序列。序列1从河流潮汐到碳酸盐岩潮汐平缓周期。序列2由盐沼为主的向上浅滩循环组成。循环的横向连续性表明低适应性内平台区域的沉积受到限制,而高台站平台边缘碳酸盐岩的堆积则逐渐增加,而长期的适应性下降的趋势。女王组包含两种储层类型: (1)由蒸发岩覆盖的硅质碎屑岩储层和(2)层状碳酸盐岩储层。在确定的四个储层区中,低水位河流三角洲沉积物中的R11具有相对较少的胶结物和最佳储层特征。

著录项

  • 作者

    Changsu, Ryu.;

  • 作者单位

    Texas A&M University.;

  • 授予单位 Texas A&M University.;
  • 学科 Geology.
  • 学位 Ph.D.
  • 年度 2002
  • 页码 212 p.
  • 总页数 212
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;
  • 关键词

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