Seismic Sequence Stratigraphic Model and Hydrocarbon Potential of Yamama Formation in Al-Fao Area, Southeastern Iraq

Q3 Earth and Planetary Sciences Iraqi Geological Journal Pub Date : 2024-01-31 DOI:10.46717/igj.57.1a.6ms-2024-1-17
Omnia Abd, Najah Abd
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Abstract

One key step when interpreting seismic reflection data is sequence stratigraphy, which has improved with well logs and seismic data. By analyzing the different layers of sediment and rock, we can better understand the geologic history of an area and make more accurate predictions for hydrocarbon exploration. The current research focuses on interpreting seismic lines from the 2D seismic surveys conducted in the Al-Fao area and data from wells in the Siba gas field to construct a stratigraphic model within the Yamama Formation, to identify hydrocarbon traps and determine the most promising zones for hydrocarbon exploration. Yamama Formation is divided into two main units representing transgressive and regressive facies deposited in highstand system tract. Six seismic facies were identified (wavy, mound shape, oblique parallel, sigmoid, chaotic, and parallel), which reflected the deposition of Yamama Formation in a ramp setting with a gentle slope. Instantaneous phase attribute was utilized, which focused on the lateral changes of seismic facies and provided detailed information about the architecture of Yamama Formation depositional basin. The results of the seismic attributes analysis included identifying carbonate buildups and progradation stacking patterns with the presence of direct hydrocarbon indicator. Three main seismic stratigraphic indexes representing potential stratigraphic traps have been identified. These three stratigraphic features reflect the facies of shoal carbonate sediments in the last depositional cycle of Yamama Formation (Highstand). The stratigraphic model showed the best image of the depositional environment of Yamama Formation that corresponds with the seismic data interpretation and identifies the promising hydrocarbon traps.
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伊拉克东南部 Al-Fao 地区 Yamama 地层的地震层序地层模型和油气潜力
解释地震反射数据的一个关键步骤是层序地层学,随着测井记录和地震数据的增加,层序地层学也得到了改进。通过分析不同的沉积层和岩石层,我们可以更好地了解一个地区的地质历史,为油气勘探做出更准确的预测。目前的研究重点是解释在 Al-Fao 地区进行的二维地震勘测的地震线和 Siba 气田的油井数据,以构建 Yamama 地层内的地层模型,识别油气陷阱并确定最有希望进行油气勘探的区域。Yamama Formation(山间地层)分为两个主要单元,分别代表在高台系统道中沉积的跃层和退层。确定了六个地震剖面(波浪形、丘状、斜平行、乙字形、混沌和平行),这些剖面反映了山间地层在坡度较缓的斜坡环境中的沉积情况。利用瞬时相位属性,重点研究了地震面的横向变化,提供了有关山间组沉积盆地结构的详细信息。地震属性分析的结果包括确定了碳酸盐岩堆积和渐变堆积模式,并发现了直接的碳氢化合物指示物。确定了代表潜在地层陷阱的三个主要地震地层指标。这三个地层特征反映了山间地层(高台)最后一个沉积周期中浅滩碳酸盐沉积的面貌。该地层模型显示了山间组沉积环境的最佳图像,与地震数据解释相吻合,并确定了有潜力的油气陷阱。
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来源期刊
Iraqi Geological Journal
Iraqi Geological Journal Earth and Planetary Sciences-Geology
CiteScore
1.80
自引率
0.00%
发文量
152
审稿时长
7 weeks
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