首页> 外文会议>Convention of the Gulf Coast Association of Geological Societies American Association of Petroleum Geologists Sectional Meeting >Reservoir Quality and Porosity-Permeability Trends in Onshore Wilcox Sandstones, Texas and Louisiana Gulf Coast:Application to Deep Wilcox Plays, Offshore Gulf of Mexico
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Reservoir Quality and Porosity-Permeability Trends in Onshore Wilcox Sandstones, Texas and Louisiana Gulf Coast:Application to Deep Wilcox Plays, Offshore Gulf of Mexico

机译:陆上Wilcox砂岩,德克萨斯州和路易斯安那州湾海岸的水库质量和孔隙率趋势:在墨西哥海上海湾的威尔科克剧中应用

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Evolution of porosity and permeability in Lower Tertiary Wilcox sandstones during burial diagenesis was evaluated using petrographic and petrophysical data from onshore sandstones of the Texas and Louisiana Gulf Coast. The results provide insight into reservoir quality of deeply buried Wilcox sandstones beneath the Gulf of Mexico shelf and in the deep Gulf. Wilcox sandstone samples used in this study were deposited in the Holly Springs Delta of Louisiana, the Houston Delta of the upper Texas coast, and the Rosita Delta of the lower Texas coast. Petrographic analysis of 534 Wilcox thin sections from 90 wells was combined with core-analysis data from >10,000 core samples from 189 wells to determine regional variation in pore-type evolution and porosity-permeability trends with increasing burial depth and temperature. Petrographic data show that Wilcox sandstone pores change from a mix of primary and secondary pores and micropores at lower temperatures to predominantly secondary pores and micropores at temperatures >300°F (150°C). Primary porosity, the most important control on permeability, decreases from an average of 40% at the time of deposition to 5-8% by 250°F (125°C) and 1-2% at temperatures >390°F (>200°C). Core-analysis data were used to calculate porosity-permeability transforms within different temperature intervals in each area. Because the sandstone pore types change with increasing temperature, porosity-permeability transforms also change; at higher temperatures, permeability is lower per porosity unit. A transform developed for low-temperature sandstones is not appropriate to use in higher-temperature sandstones. At temperatures >212°F (100°C), Wilcox sandstones in the Houston Delta System have lower permeability for a given porosity than sandstones in the Holly Springs and Rosita delta systems. These data suggest that high-temperature Wilcox sandstones beneath the present shelf and in the deep Gulf that were sourced by the Holly Springs and Rosita deltas may have better reservoir quality than do sandstones derived from the Houston Delta.
机译:从德克萨斯州德克萨斯州和路易斯安那州湾海岸的陆上砂岩的岩体和岩石物理数据评估埋藏成岩作用期间孔隙率和渗透率的渗透性和渗透性。结果提供了对墨西哥湾海湾和深海湾的深埋Wilcox砂岩的水库质量的洞察力。本研究中使用的Wilcox砂岩样品被沉积在Louisiana的Holly Springs Delta,位于德克萨斯州的上部河岸的休斯顿三角洲,以及德克萨斯州下德克萨斯州的Rosita Delta。从199孔的90孔中的534个Wilcox薄片的岩体分析与来自189孔的10,000核样品的核心分析数据结合,以确定孔型演化和孔隙率渗透率趋势的区域变异,随着墓穴深度和温度。岩体数据表明,Wilcox砂岩孔孔隙从初级和次级孔隙和微孔的混合变化,在较低的温度下,在温度> 300°F(150°C)时主要孔和微孔。初级孔隙率,最重要的渗透性控制,在沉积时的平均40%降低至5-8%(125℃),在温度下1-2%> 390°F(> 200 °C)。核心分析数据用于计算每个区域的不同温度间隔内的孔隙率磁性变换。因为砂岩孔隙类型随着温度的增加而变化,孔隙率渗透性变化也会发生变化;在较高的温度下,每个孔隙率单位渗透性降低。为低温砂岩开发的变换不适用于高温砂岩。在温度> 212°F(100°C)中,休斯顿三角洲系统中的Wilcox砂岩具有比冬青弹簧和Rosita Delta系统中的给定孔隙率的渗透率较低。这些数据表明,当前架子和霍利斯塔斯蒂斯源的高温Wilcox砂岩和霍尔塔斯蒂斯德塔斯来源的深鸿沟可能具有比休斯顿三角洲衍生的砂岩更好的储层质量。

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