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Trapped Fluid Analysis of 58 Wells from the SCOOP and STACK Plays, Oklahoma

机译:俄克拉荷马州的勺子和堆栈剧中捕获了58个井的流体分析

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Archived cuttings samples (n = 6713) from 58 wells located in the SCOOP and STACK plays of the Anadarko Basin in Oklahoma (Figure 1; Table 1) were analyzed for their bulk trapped fluid content (fluid inclusions and other tightly held volatiles) via the fluid inclusion stratigraphy (FIS) technique. Fluid inclusion petrography (n = 300) and microthermometry (n '= 58) analyses were also performed on selected intervals, based on FIS results. Data were used to evaluate the vertical and lateral distribution of hydrocarbons and non-hydrocarbon volatiles, oil gravities, phase state, salinity, and burial temperatures. The most prominent gas and liquid hydrocarbon FIS responses are recorded in the Caney to Viola sections. Both migrated and locally generated components are distinguished, and several episodes of migration may be documented within a given well. Overall, FIS oil/condensate responses and petrographic observations suggest a liquids-enhanced interval at 8,000-12,000 ft, although in some instances liquid petroleum zones extend to 15,000 ft. Gas-enrichment occurs to the west in response to increased thermal maturity, and sulfur species related to thermochemical sulfate reduction at high temperature occur towards the west and at depths >13,000 ft. Measured petroleum inclusions show mostly values of 38° to 45° API gravity. Most petroleum inclusions homogenize via bubble-point transition, and bubble-point temperatures suggest that they occur as undersaturated liquids at current reservoir conditions. Aqueous inclusion homogenization temperatures (T_h) imply maximum burial temperatures that are generally higher than current temperatures, and probably reflect 3000-4000 ft of uplift since inclusion formation. Inclusion salinities are generally in the 1-5 weight percent NaCl-equivalent range suggesting brackish to evolved basin fluids. Independent measures of thermal maturity, including pyrolysis, T_h of aqueous inclusions, and biomarkers, are in general agreement, and suggest that much of the recorded petroleum was proximally sourced. This historically productive region is attractive for unconventional reservoir development due to liquids potential and favorable economics. However, fluid characteristics can vary greatly over a relatively small area, resulting in significant differences in recovery from nearby wells. By analyzing fluid inclusions, it is possible to establish regional hydrocarbon potential with a small amount of unpreserved, archived drill cuttings and evaluate the likely production characteristics of fluids within a given area.
机译:从位于俄克拉荷马州的勺子和堆栈播放的58孔中的存档切割样品(n = 6713)(图1;表1)分析其散装捕获的液体含量(流体夹杂物和其他紧紧持有的挥发物)通过流体夹杂物层(FIS)技术。基于FIS结果,还对所选间隔进行流体包容岩体(n = 300)和微摩体(n'= 58)分析。数据用于评估烃和非烃挥发物,油重力,相状态,盐度和龈缘的垂直和横向分布。最突出的气体和液态碳氢化合物FIS响应记录在Caney到中提琴部分。分辨迁移和本地生成的组件,并且可以在给定的井中记录几个迁移剧集。总体而言,FIS油/冷凝物反应和岩体观察表明液体增强的间隔为8,000-12,000英尺,虽然在某些情况下,液体石油区延伸至15,000英尺。在响应热成熟度和硫的增加时,富集气体富集。在高温下的热化学硫酸盐降低有关的物种,朝向西部和深度> 13,000英尺。测量的石油夹杂物显示出38°至45°重力的大部分。大多数石油夹杂物通过气泡点转变均匀化,气泡点温度表明它们在电流储层条件下发生较缺的液体。含水包涵体均匀化温度(T_H)意味着通常高于当前温度的最大粗缘温度,并且由于包涵体形成,可能反映了3000-4000英尺的隆起。包含盐度通常在1-5重量%的NaCl-等效范围内,表明进化盆腔流体脆皮。综合协议,包括热成熟度,包括热解,含水夹杂物和生物标志物的独立措施,并建议近距离循环多大的记录石油。由于液体潜在和有利的经济学,这一历史上生产的地区对于非传统的水库开发具有吸引力。然而,流体特性可以在相对较小的面积上变化很大,导致附近井中的恢复显着差异。通过分析流体夹杂物,可以通过少量未验证的,存档的钻头切屑建立区域烃电位,并评估给定区域内的流体的可能生产特性。

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