Quantifying the lateral heterogeneity of distal submarine lobe deposits, Point Loma Formation, California: Implications for subsurface lateral facies prediction

IF 1.9 3区 地球科学 Q1 GEOLOGY
Kaci B. Kus, Zane R. Jobe, Fabien Laugier, Wylie Walker, Morgan Sullivan
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引用次数: 1

Abstract

Submarine fan deposits are volumetrically the largest sediment accumulations on Earth and host significant hydrocarbon reserves. Extensive research has documented the bed-scale architecture of high sand-to-mud ratio, proximal and axial environments, which can have bed thicknesses of several metres; however, less well-understood are thin-bedded turbidites, which are typically lower N:G and deposited in more distal environments. Conceptual models assume that lobe-fringe-to-basin plain environments consist of tabular, sheet-like beds that extend out continuously and predictably over long distances—up to several kilometres. Extensive lateral continuity, however, is not necessarily reflected in ancient outcrop analogues. This study seeks to apply a quantitative approach to the characterisation of thin-bedded turbidites to assess the impact of multi-scale heterogeneity on reservoir predictability. The sea-cliff outcrop exposures of the Upper Cretaceous Point Loma Formation in San Diego, California, exhibit a wide range of bed thicknesses and stratigraphic architecture, which have been used to interpret an off-axis-to-fringe depositional environment. The study area spans 700 m of laterally continuous outcrop, across which 10 correlated stratigraphic sections are used to quantify changes in metrics such as bed thickness, N:G, lithofacies proportions, etc. Results of this study demonstrate that thin sand beds experience both lateral facies changes and rapid thickness changes more frequently than conceptual models would predict. A single measure of lateral heterogeneity does not reflect the true architecture of sandstone beds, and significant information is lost when beds are correlated over ten to hundreds of metres. Sands are commonly deposited in irregular, ‘finger-like’, planform geometries, which compounds at the lobe element scale and influences lateral lithofacies predictability. This study of the Point Loma Formation offers high-resolution bed-to-element scale data, which may be used as inputs for reservoir models and horizontal facies predictions in both conventional and unconventional hydrocarbon reservoirs.

Abstract Image

量化加利福尼亚洛马点组远海底叶状沉积的横向非均质性:地下横向相预测的意义
海底扇沉积是地球上体积最大的沉积物堆积,拥有重要的碳氢化合物储量。广泛的研究记录了高砂泥比、近端和轴向环境的床级结构,其床层厚度可达数米;然而,人们对薄层浊积岩知之甚少,它们通常具有较低的N:G,沉积在较远的环境中。概念模型假设叶状边缘到盆地的平原环境由板状、片状的床组成,这些床可以连续地、可预测地向外延伸,最长可达数公里。然而,广泛的横向连续性并不一定反映在古代的类似露头中。本研究旨在应用定量方法来表征薄层浊积岩,以评估多尺度非均质性对储层可预测性的影响。加利福尼亚圣地亚哥上白垩统Point Loma组的海崖露头显示出广泛的地层厚度和地层结构,这被用来解释离轴到边缘的沉积环境。研究区横向连续露头700 m,利用10个相关地层剖面量化了层厚、N:G、岩相比例等指标的变化。研究结果表明,薄砂层经历横向相变化和快速厚度变化的频率比概念模型预测的要高。横向非均质性的单一测量并不能反映砂岩层的真实结构,当层在10到数百米的高度上进行对比时,重要的信息就丢失了。砂体通常呈不规则的、“指状”的台地几何形状,这些形状在叶状单元尺度上混合在一起,影响了侧向岩相的可预测性。对Point Loma地层的研究提供了高分辨率的层元尺度数据,可作为常规和非常规油气藏储层模型和水平相预测的输入。
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来源期刊
CiteScore
4.10
自引率
16.70%
发文量
42
审稿时长
16 weeks
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