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首页> 外文期刊>AAPG Bulletin >Evidence for a petroleum subsystem in the Frontier Formation of the Uinta-Piceance Basin petroleum province
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Evidence for a petroleum subsystem in the Frontier Formation of the Uinta-Piceance Basin petroleum province

机译:Uinta-Piceance盆地石油省边界层中一个石油子系统的证据

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摘要

Anomalous carbonate horizons with intercrystalline hydrocarbon residue, cone-in-cone structures, and calcite "beef" veins in adjacent sandstone beds record potential evidence for hydrocarbon generation and seepage in the middle to upper Turonian Frontier Formation from the Uinta Basin, Utah and Colorado. Eight carbonate occurrences, all encountered within distal delta-front facies (thin-bedded sandstones and siltstones), were sampled at outcrop locations from the southern and eastern margins of Dinosaur National Monument. Seven petrographic facies (PF1-PF7) were identified using standard petrographic and cathodoluminescence microscopy: PF1, large and small botryoids and fans; PF2, yellow-brown spherules; PF3, microcrystalline spar cement; PF4, blocky spar; PF5, prismatic spar; PF6, drusy mosaic spar; and PF7, dolomite. Facies PF1-PF3 are synsedimentary phases comprising a large percentage of carbonate horizon volume, whereas PF4-PF7 are late-stage fabrics. The delta C-13 values of PF1-PF3 (-9.9 parts per thousand to -20.0 parts per thousand) are consistent with contributions from biogenic methane seepage during deposition and early diagenesis. Brecciated PF1 fabrics and blowout depressions within sandstone horizons further indicate significant methane generation during deposition and early burial. Late-stage fabrics contain delta C-13 (-8.0 parts per thousand to -17.3 parts per thousand) and delta O-18 (-6.5 parts per thousand to -13.5 parts per thousand) values consistent with progressive burial, during which intercrystalline hydrocarbon residue, cone-in cone structures, and calcite beef veins were formed by the thermal maturation of organic matter from enclosing distal delta-front facies. Together, these features reveal the potential for the thin bedded facies of the Frontier Formation distal delta front to serve as a potentially viable petroleum subsystem previously unrecognized in the Uinta-Piceance petroleum province.
机译:碳酸盐岩异常层位具有晶间烃残留物,圆锥体结构和相邻砂岩层中的方解石“牛肉”脉,记录了从尤因塔盆地,犹他州和科罗拉多州开始的中至上图龙盆地边界层中油气生成和渗漏的潜在证据。在恐龙国家纪念碑南缘和东缘的露头位置采样了八次碳酸盐岩,全部发生在三角洲前缘相(薄层砂岩和粉砂岩)中。使用标准的岩相和阴极发光显微镜鉴定了七个岩相(PF1-PF7):PF1,大,小葡萄状和扇形; PF2,黄褐色小球; PF3,微晶石水泥; PF4,块状晶石; PF5,棱柱晶石; PF6,杂色晶石;和PF7,白云石。 PF1-PF3相是含大量碳酸盐岩视界体积的沉积相,而PF4-PF7是后期织物。 PF1-PF3的C-13增量值(-9.9千分之至-20.0千分之几)与沉积和早期成岩过程中生物甲烷渗透的贡献一致。 PF1织物的角化和砂岩地层内的井喷凹陷进一步表明在沉积和早期埋藏过程中会大量产生甲烷。后期织物的δC-13(-8.0千分之一至-17.3千分之一)和δO-18(-6.5千分之一至-13.5千分之三)的值与逐步埋葬一致,在此期间晶间碳氢化合物残留的三角洲前缘相通过有机质的热成熟形成了残留物,锥形锥体结构和方解石牛肉脉。这些特征共同揭示了边界层远端三角洲锋面的薄层相可能成为先前在Uinta-Piceance石油省中未被发现的潜在可行的石油子系统。

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