Seismic stratigraphic analysis of the Pre-salt of Berbigão, Sururu, and Atapu fields, Santos Basin, Brazil

IF 3.6 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Victor Haas Pizarro , Fábio André Perosi , Leonardo Borghi , Marcos Fetter
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Abstract

The Pre-salt section of Santos Basin, formed during the Lower Cretaceous, hosts one of the world's most significant hydrocarbon provinces, yet its complex carbonate reservoirs are yet to be fully understood. This study consists of a seismic analysis and interpretation of the Pre-salt interval of Berbigão, Sururu, and Atapu fields, focusing on the Upper Barra Velha Formation. A 3D seismic volume and sixteen wells were analyzed. At the Pre-salt level, five seismic units were defined. Distinct seismic facies were described and mapped throughout the Sag unit. These seismic facies were analyzed for occurrence patterns and incorporated with data from lithofacies and electrofacies. It was concluded that seismic facies Parallel corresponds to carbonate platforms principally composed of spherulitestone and mudstone variations and developed in both high- and low-energy sublittoral lake zones. Seismic facies Divergent Wedge and Fill represent profundal sediments deposited in deeper portions of the lake, where a higher concentration of organic-rich shales and mudstones would occur. This element is often associated with syndepositional faulting in the Sag unit. Seismic facies Mound represents carbonate mounds predominantly composed of shrubstone variations and shrubby spherulitestones. They occur along deep-seated faults and contain conspicuous amounts of silica and uranium. Mounds likely formed in intermediate to shallow sublittoral zones, being occasionally subjected to subaerial exposure. The formation and enrichment of these carbonate mounds are likely associated with hydrothermal processes, where faults would have acted as conduits for the percolation of hydrothermal fluids. Significant concentrations of shrubs in the Upper Barra Velha Formation are probably related to carbonate precipitation from hydrothermal fluids. The interpretations derived from this integrated study provide new insights into reservoir heterogeneity in the Upper Barra Velha, with direct implications for reservoir prediction, well placement, and production optimization in similar Pre-salt settings.
巴西Santos盆地berbigo、Sururu和Atapu油田盐下地震地层分析
Santos盆地盐下部分形成于下白垩纪,是世界上最重要的油气产区之一,但其复杂的碳酸盐岩储层尚未被完全了解。本研究包括对berbig、Sururu和Atapu油田盐下段的地震分析和解释,重点是上Barra Velha组。对16口井的三维地震体进行了分析。在盐下水平,确定了5个地震单元。在整个凹陷单元中描述并绘制了不同的地震相。对这些地震相的产状进行了分析,并与岩相和电相资料相结合。地震相平行对应于以球晶岩和泥岩变异为主的碳酸盐岩台地,发育于高、低能滨下湖区。地震相发散楔形和填充代表了沉积在湖泊较深部分的深层沉积物,在那里会出现高浓度的富有机质页岩和泥岩。该元素通常与凹陷单元的同沉积断裂有关。地震相丘为以灌木状变异体和灌木状球粒岩为主的碳酸盐岩丘。它们沿深层断层而生,含有大量的二氧化硅和铀。土丘可能形成于中浅海下地带,偶尔受到陆上暴露。这些碳酸盐岩丘的形成和富集可能与热液作用有关,其中断层可能是热液流体渗透的管道。上巴拉Velha组灌木的显著富集可能与热液流体的碳酸盐沉淀有关。这项综合研究的解释为Upper Barra Velha的储层非均质性提供了新的见解,对类似盐下环境的储层预测、井位和生产优化具有直接意义。
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来源期刊
Marine and Petroleum Geology
Marine and Petroleum Geology 地学-地球科学综合
CiteScore
8.80
自引率
14.30%
发文量
475
审稿时长
63 days
期刊介绍: Marine and Petroleum Geology is the pre-eminent international forum for the exchange of multidisciplinary concepts, interpretations and techniques for all concerned with marine and petroleum geology in industry, government and academia. Rapid bimonthly publication allows early communications of papers or short communications to the geoscience community. Marine and Petroleum Geology is essential reading for geologists, geophysicists and explorationists in industry, government and academia working in the following areas: marine geology; basin analysis and evaluation; organic geochemistry; reserve/resource estimation; seismic stratigraphy; thermal models of basic evolution; sedimentary geology; continental margins; geophysical interpretation; structural geology/tectonics; formation evaluation techniques; well logging.
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