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首页> 外文期刊>Journal of African earth sciences >Petroleum system elements within the Late Cretaceous and Early Paleogene sediments of Nigeria's inland basins: An integrated sequence stratigraphic approach
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Petroleum system elements within the Late Cretaceous and Early Paleogene sediments of Nigeria's inland basins: An integrated sequence stratigraphic approach

机译:尼日利亚内陆盆地晚白垩世和古近纪早期沉积物中的石油系统元素:综合层序地层学方法

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Sequence stratigraphic studies have been carried out using subsurface well and 2D seismic data in the Late Cretaceous and Early Paleogene sediments of Anambra and proximal onshore section of Niger Delta Basin in the Southeastern Nigeria. The aim was to establish the stratigraphic framework for better understanding of the reservoir, source and seal rock presence and distribution in the basin. Thirteen stratigraphic bounding surfaces (consisting of six maximum flooding surfaces - MFSs and seven sequence boundaries SBs) were recognized and calibrated using a newly modified chronostratigraphic chart. Stratigraphic surfaces were matched with corresponding foraminiferal and palynological biozones, aiding correlation across wells in this study. Well log sequence stratigraphic correlation reveals that stratal packages within the basin are segmented into six depositional sequences occurring from Late Cretaceous to Early Paleogene age. Generated gross depositional environment maps at various MFSs show that sediment packages deposited within shelfal to deep marine settings, reflect continuous rise and fall of sea levels within a regressive cycle. Each of these sequences consist of three system tracts (lowstand system tract LST, transgressive system tract - TST and highstand system tract - HST) that are associated with mainly progradational and retrogradational sediment stacking patterns. Well correlation reveals that the sand and shale units of the LSTs, HSTs and TSTs, that constitute the reservoir and source/seal packages respectively are laterally continuous and thicken basinwards, due to structural influences. Result from interpretation of seismic section reveals the presence of hanging wall, footwall, horst block and collapsed crest structures. These structural features generally aid migration and offer entrapment mechanism for hydrocarbon accumulation. The combination of these reservoirs, sources, seals and trap elements form a good petroleum system that is viable for hydrocarbon exploration and development. (C) 2017 Elsevier Ltd. All rights reserved.
机译:利用地下井和二维地震数据,在尼日利亚东南部阿南布拉的白垩纪晚期和古近纪早期沉积以及尼日尔三角洲盆地近岸陆上段进行了层序地层研究。目的是建立地层学框架,以更好地了解盆地中的储层,烃源和盖层岩石的存在与分布。使用新修改的年代地层图识别并校准了13个地层边界面(由6个最大洪泛面-MFS和7个层序边界SB组成)。地层表面与相应的有孔虫和孢粉生物区相匹配,在本研究中有助于各井之间的相关性。测井序列地层相关性揭示,盆地内的地层包裹被分为从白垩纪晚期到古近纪早期的六个沉积层序。在不同的MFS上生成的总沉积环境图表明,在陆架到深海环境中沉积的沉积物包反映了回归周期内海平面的连续上升和下降。这些序列中的每一个序列均由三个系统区组成(低位系统区LST,海侵系统区-TST和高位系统区-HST),它们主要与累积和回生沉积物堆积模式有关。良好的相关性表明,由于结构的影响,分别构成储集层和源/盖层组合的LST,HST和TST的砂岩和页岩单元在横向上是连续的,在盆地上是增稠的。地震剖面解释的结果表明存在悬壁,下盘,霍斯特块和坍塌的波峰结构。这些结构特征通常有助于迁移,并为碳氢化合物的聚集提供了诱集机制。这些储层,烃源,密封和圈闭要素的组合形成了一个良好的石油系统,可用于烃类勘探和开发。 (C)2017 Elsevier Ltd.保留所有权利。

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