首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Multiple atmospheric noble gas components in hydrocarbon reservoirs: A study of the Northwest Shelf, Delaware Basin, SE New Mexico
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Multiple atmospheric noble gas components in hydrocarbon reservoirs: A study of the Northwest Shelf, Delaware Basin, SE New Mexico

机译:油气藏中的多种大气稀有气体成分:新墨西哥州东南部特拉华盆地西北大陆架的研究

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The Northwest Shelf of the Delaware Basin, SE New Mexico is the site of several large and productive oil and gas fields. The most productive reservoirs are located in the late Pennsylvanian Morrow and early Permian Abo formations. Production from the latter more important play is predominately from fluvial Abo red beds of the Pecos Slope Field. The oxidizing conditions implied by the reddish color of the formation require an external hydrocarbon source. To test the existing migration model for the region and constrain the location of potential hydrocarbon sources, we measured the elemental and isotopic composition of noble gases produced along with the hydrocarbons. We found the hydrocarbons to be highly enriched in radiogeniC He-4, Ar-40* and nucleogeniC Ne-21* [F(He-4) = 44,000-250,000; Ar-40/Ar-36 = 400-3145; Ne-21/Ne-22 = 0.044-0.071]. The greatest enrichments occur in the Pecos Slope gas fields. The hydrocarbons also contain three independent nonradiogenic noble gas components each with an atmospheric isotopic composition. One component is most likely air-saturated water (ASW). The second component is enriched in the heavy noble gases [F(Xe-130) > 8.5] and is derived from the hydrocarbon sources. The third component is enriched in Ne [F(Ne-20) > 0.8] that we believe is degassed from sources within the reservoirs. This component is correlated with but decoupled from the dominant source of radiogenie He-4 and Ar-40*. Very high concentrations of He-4 (up to similar to1% by volume) in the Pecos slope reservoirs require a source external to the reservoirs, such as the underlying Precambrian basement granites and sedimentary equivalents. Structural buckles cutting through the Pecos field may act as high flux vertical pathways for the radiogeniC 4 He. If the hydrocarbons in the Pecos slope fields have migrated northward from the deeper Delaware Basin, as suggested by compositional trends, then perhaps the buckles also play an important role in the distribution and filling of the Pecos slope reservoirs. Copyright (C) 2002 Elsevier Science Ltd. [References: 42]
机译:新墨西哥州东南部特拉华盆地的西北大陆架是几个大型生产性油气田的所在地。生产力最高的储层位于宾夕法尼亚州的莫罗晚期和二叠纪阿波早期。后一个更重要的戏剧的生产主要来自Pecos Slope油田的河流Abo红层。地层的红色暗示的氧化条件需要外部烃源。为了测试该地区的现有运移模型并限制潜在烃源的位置,我们测量了与烃一起产生的稀有气体的元素和同位素组成。我们发现碳氢化合物高度富集于放射原He-4,Ar-40 *和核原Ne-21 * [F(He-4)= 44,000-250,000; Ar-40 / Ar-36 = 400-3145; Ne-21 / Ne-22 = 0.044-0.071]。最大的富集发生在Pecos Slope气田中。烃还包含三种独立的非放射性稀有气体组分,每种组分均具有大气同位素组成。一种成分是最有可能的空气饱和水(ASW)。第二种成分富含重质稀有气体[F(Xe-130)> 8.5],并且源自烃类来源。第三个成分富含Ne [F(Ne-20)> 0.8],我们认为这是从储层中的气源中脱气的。该成分与放射源He-4和Ar-40 *的主要来源相关但不相关。 Pecos斜坡储层中的He-4浓度很高(高达约1%(体积)),需要储层外部的来源,例如底层的前寒武纪基底花岗岩和沉积等价物。穿过Pecos场的结构性弯折可能充当radiogeniC 4 He的高通量垂直路径。如果Pecos斜坡油田中的碳氢化合物已从组成趋势上暗示从较深的特拉华盆地向北迁移,那么弯曲可能在Pecos斜坡油藏的分布和填充中也起着重要作用。版权所有(C)2002 Elsevier Science Ltd. [参考:42]

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