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首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Integrated geophysical and geological study and petroleum appraisal of Cretaceous plays in the Western Gulf of Gabes, Tunisia
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Integrated geophysical and geological study and petroleum appraisal of Cretaceous plays in the Western Gulf of Gabes, Tunisia

机译:突尼斯加贝斯西湾白垩纪油气田的综合地球物理和地质研究以及石油评估

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摘要

An integrated study of available seismic and calibrated wells has been conducted in order to ascertain the structural development and petroleum potential of the Cretaceous Formations of the Western Gulf of Gabes. This study has resulted in an understanding of the controls of deep seated Tethyan tectonic lineaments by analysis of the Cretaceous deposits distribution. Three main unconformities have been identified in this area, unconformity U1 between the Jurassic and Cretaceous series, unconformity U2 separating Early from Late Cretaceous and known as the Austrian unconformity and the major unconformity U3 separating Cretaceous from Tertiary series. The seismic analysis and interpretation have confirmed the existence of several features dominated by an NE-SW extensive tectonic regime evidenced by deep listric faults, asymmetric horst and graben and tilted blocks structures. Indeed, the structural mapping of these unconformities, displays the presence of dominant NW-SE fault system (N140 to N160) bounding a large number of moderate sized basins. A strong inversion event related to the unconformity U3 can be demonstrated by the mapping of the unconformities consequence of the succession of several tectonic manifestations during the Cretaceous and post-Cretaceous periods. These tectonic events have resulted in the development of structural and stratigraphic traps further to the porosity and permeability enhancement of Cretaceous reservoirs. (C) 2015 Elsevier B.V. All rights reserved.
机译:为了确定加贝角西部海湾白垩纪地层的结构发育和石油潜力,已经对可用的地震井和标定井进行了综合研究。这项研究通过分析白垩纪沉积物的分布,使人们了解了深层特提斯构造构造的控制。在该地区已经发现了三个主要不整合面,侏罗纪和白垩纪系列之间的不整合面U1,早白垩世之间的不整合面U2(称为奥地利不整合面)和白垩纪与第三纪系列之间的主要不整合面U3。地震分析和解释已经证实了以东北—西南广泛的构造体制为主导的几个特征的存在,这些特征以深的断层断层,不对称的地心,grab陷和倾斜的块体结构为证据。的确,这些不整合面的构造图显示了主要的西北-东南断层系统(N140至N160)的存在,该断层系统限制了许多中等大小的盆地。与不整合面U3有关的强烈反演事件可以通过对白垩纪和后白垩纪时期几种构造表现的演替的不整合面结果进行映射来证明。这些构造事件导致了结构和地层圈闭的发展,进一步提高了白垩纪储层的孔隙度和渗透率。 (C)2015 Elsevier B.V.保留所有权利。

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