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Lacustrine carbonate reservoirs from Early Cretaceous rift lakes of Western Gondwana: Pre-Salt coquinas of Brazil and West Africa

机译:冈瓦纳西部早白垩世裂谷湖的湖相碳酸盐岩储层:巴西和西非的盐前海藻

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Barremian-Aptian (Lower Cretaceous) Pre-Salt lacustrine carbonates host large petroleum reservoirs in South Atlantic rift basins, yet remain poorly studied, in part due to the scarcity of lacustrine carbonate reservoirs throughout the geological record. This review provides an integrated discussion of the current state of knowledge on the coquina play, having been deposited in extensive rift lakes during the early stages of the opening of the South Atlantic. Thick successions of coquina are recorded from the Santos to Sergipe-Alagoas basins and the Kwanza to Gabon basins on the Brazilian and West African continental margins, respectively. Coquinas exhibit similarities in depositional processes across the South Atlantic, however, have distinct diagenetic histories and stratigraphic stacking patterns, having been deposited in lakes with different geologies, climates and water chemistries. West African coquinas exhibit depositional characteristics that are indicative of deposition on distally steepened ramps and rimmed platforms, and accordingly, facies are somewhat different to those in Brazilian basins, which were deposited on low angle ramps. As petroleum exploration continues into ultra-deep waters on the Brazilian and West African margins, accurate facies models will be important for the predictability of carbonate reservoir intervals. To this end, onshore outcrop in the Sergipe-Alagoas Basin has revealed that the molluscan faunas have marine origins, suggesting that facies patterns may be more complex than previously considered. It is hoped that this review will provide the impetus for further research on the coquinas, especially given the presence of poorly studied, easily accessible onshore outcrops. (C) 2015 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
机译:巴里米亚-阿普特(下白垩统)盐下的湖相碳酸盐岩在南大西洋裂谷盆地中拥有大量的石油储层,但仍缺乏研究,部分原因是整个地质记录中湖相碳酸盐岩储层的稀缺性。这篇综述提供了有关对喹啉亚砜的当前知识状态的综合讨论,该知识在南大西洋开放初期已沉积在广阔的裂谷湖中。在巴西和西非大陆边缘,从桑托斯盆地到塞尔吉普-阿拉戈斯盆地以及宽扎盆地到加蓬盆地,分别记录了厚厚的连续藜。 Coquinas在整个南大西洋的沉积过程中表现出相似性,但是具有不同的成岩历史和地层堆积模式,沉积在具有不同地质,气候和水化学特征的湖泊中。西非洋藜具有沉积特征,表明沉积在远端陡峭的斜坡和有缘平台上,因此,相与巴西盆地的相有些不同,后者沉积在低角度斜坡上。随着石油勘探继续进入巴西和西非边缘的超深水域,准确的岩相模型对于碳酸盐岩储层间隔的可预测性将至关重要。为此,塞尔吉普-阿拉戈斯盆地的陆上露头表明,软体动物群具有海洋起源,这表明相图型可能比以前认为的更为复杂。希望这次审查将为进一步研究蓝藻提供动力,特别是考虑到存在研究不足,易于接近的陆上露头的情况。 (C)2015年冈瓦纳国际研究协会。由Elsevier B.V.发布。保留所有权利。

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