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Seismic reflection imaging of karst in the Persian Gulf; Implications for the characterization of carbonate reservoirs

机译:波斯湾喀斯特地震反射成像;对碳酸盐岩储层特征的影响

摘要

Karstification positively and negatively affects the quality of carbonate reservoirs; for example, dissolution and brecciation can increase porosity and permeability, whereas cavern collapse or cementation driven by postkarstification fluid flow may occlude porosity and reduce permeability. Karst may also pose challenges to drilling because of the unpredictable and highly variable porosity and permeability structure of the rock and the corresponding difficulty in predicting drilling mud weight. When combined, outcrop, petrographic, and geochemical data can constrain the style, distribution, and origin of seismic-scale karst, which may provide an improved understanding of carbonate reservoir architecture and allow development of safer drilling programs. However, relatively few studies have used seismic reflection data to characterize the regional development of seismic-scale karst features. In this study we use time-migrated two-dimensional seismic reflection data to determine the distribution, scale, and genesis of karst in a 3-km-thick (9800-ft-thick), Jurassic–Miocene carbonate-dominated succession in the Persian Gulf. We map 43 seismic-scale karst features, which are expressed as vertical pipe columns of chaotic reflections capped by downward-deflected depressions that are onlapped by overlying strata. The columns are up to 2 km (6500 ft) tall, spanning the Upper Jurassic to Upper Cretaceous succession, and are up to 5.5 km (18,000 ft) in diameter. We interpret these pipes to have formed in response to hypogene karstification by fluids focused along preexisting faults, with hypogene-generated depressions enhanced by epigene processes during key intervals of exposure. Our study indicates that seismic reflection data can and should be used in conjunction with petrographic and geochemical techniques to determine the presence of hypogene karst plays and to help improve the characterization of carbonate reservoirs and associated drilling hazards.
机译:岩溶作用对碳酸盐岩储层的质量有正反作用。例如,溶解和成岩作用可以增加孔隙度和渗透率,而岩溶后流体流动驱动的洞穴塌陷或胶结作用可能会堵塞孔隙并降低渗透率。由于岩石的孔隙度和渗透率结构不可预测且高度可变,并且在预测钻探泥浆重量方面存在相应的困难,因此岩溶也可能给钻井带来挑战。结合使用时,露头,岩相和地球化学数据可以限制地震规模的喀斯特地貌,分布和成因,从而可以更好地理解碳酸盐岩储层的构造并允许开发更安全的钻探程序。但是,很少有研究使用地震反射数据来表征地震规模的岩溶特征的区域发展。在这项研究中,我们使用时间偏移的二维地震反射数据来确定波斯地区3公里厚(9800英尺厚),侏罗系中新世碳酸盐岩为主的演替过程中的岩溶分布,规模和成因。海湾。我们绘制了43个地震规模的喀斯特地貌,这些地貌表示为由向下反射的凹陷所覆盖的混沌反射的垂直管柱,这些凹陷由上覆的地层重叠。这些柱高达2公里(6500英尺),横跨上侏罗纪至上白垩统,直径最大为5.5公里(18,000英尺)。我们将这些管道解释为响应沿先生断裂集中的流体对次生岩溶作用而形成,在关键的暴露时间间隔内,由表观遗传过程增强了次生岩生的凹陷。我们的研究表明,地震反射数据可以并且应该与岩相学和地球化学技术结合使用,以确定是否存在次生岩溶岩溶岩,并有助于改善碳酸盐岩储层的特征和相关的钻井危害。

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