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首页> 外文期刊>Sedimentary geology >Pilot study on provenance and depositional controls on clay mineral coatings in active fluvio-eolian systems, western USA
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Pilot study on provenance and depositional controls on clay mineral coatings in active fluvio-eolian systems, western USA

机译:美国活性氟虫 - Eolian系统中粘土矿物涂料的出差和沉积对照的试验研究

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Understanding the distribution of grain coating minerals in sandstones may be crucial in evaluating the reservoir quality of deeply buried lithologies since they can inhibit syntaxial overgrowth cementation and thus preserve intergranular pore space. In unconsolidated sediments, the presence of clay mineral grain coatings and their coverage are often related to the depositional subenvironment, grain size, sorting, and skewness. These properties are interpreted to reflect the amount of clay minerals present to form coatings and relate to sediment transport and reworking. Samples from three active fluvio-eolian depositional systems in the USA (Mesquite Flat Sand Dunes, near Stovepipe Wells, CA; Algodones Dunes, near Brawley, CA; and Coral Pink Sand Dunes, near Kanab, UT) were studied using petrography (transmitted light and SEM) and XRD analyses to test and apply the available correlations to fluvio-eolian sediment samples. The frequently used correlations to the depositional subenvironment, grain size. sorting, and skewness only show poor fits (R-2 0.25). Highest grain coating coverages are present in fluvial channels near Algodones Dunes (81%). Remobilization and abrasion lead to slightly reduced average grain coating coverages (47%) in eolian deposits located in the transition zone to the main dune field. Deposits within the main dune field show smaller average grain coating coverages (29%). Sediments supplied from a limestone rich provenance in Mesquite Flat Sand Dunes contain grain coating coverages in a range from 20 to 42%. In Coral Pink Sand Dunes sediments sourced from mature Jurassic Navajo sandstones contain the smallest average grain coating coverages (15%) indicating that source rock maturity and composition can control the coating coverage. The sediment source area and the proximity to areas where clay mineral coated grains are formed are interpreted to be the main controls on inherited grain coating coverages in the studied recent fluvio-eolian deposits. (C) 2020 Elsevier B.V. All rights reserved.
机译:了解砂岩中籽粒涂层矿物的分布可能对评估深层埋藏岩性的储层质量至关重要,因为它们可以抑制句子过度生长,从而保持晶状体孔隙空间。在未溶解的沉积物中,粘土矿物涂料及其覆盖的存在通常与沉积细胞,晶粒尺寸,分类和偏斜有关。这些性质被解释为反映存在于形成涂层并涉及沉积物运输和再加工的粘土矿物的量。来自美国的三个活性氟虫 - Eolian沉积系统的样本(Mesquite Flat Sand沙丘,靠近Stovepipe Wells,CA;避难区沙丘,CA附近,CA;和珊瑚粉红色沙丘,在Kanab附近,UT)进行了研究(传播光和SEM)和XRD分析以测试和应用与Fluvio-Eolian沉积物样本的可用相关性。经常使用与沉积细胞,晶粒尺寸的相关性。排序,偏斜仅显示差(R-2 <0.25)。最高的谷物涂层覆盖范围存在于避风音沙丘附近的河流通道中(81%)。重新化和磨损导致位于过渡区的Eolian沉积物(47%)略微减少到主要沙丘场。主要沙丘场内的矿床显示较小的平均谷物涂层覆盖范围(29%)。在Mesquite Flat Sand Sunes中的石灰石丰富的物质源供应的沉积物含有谷物涂层覆盖率,范围为20至42%。在珊瑚粉红色沙丘上,来自成熟的侏罗纪Navajo砂岩的沉积物含有最小的平均谷物涂层覆盖范围(15%),表明源岩成熟度和组合物可以控制涂层覆盖率。沉积物源区和邻近形成粘土矿物涂层晶粒的区域被解释为近期氟维奥沉积物中遗传晶粒涂层覆盖物的主要对照。 (c)2020 Elsevier B.v.保留所有权利。

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