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Tectonic Map of Abu Dhabi, UAE

机译:阿布扎比,阿联酋的构造图

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The study of tectonics deals with the broad architecture of the outer part of the Earth, the age, relationship, evolution of regional structural, deformational, and crustal features. Subsurface geological maps are perhaps the most important tool used to explore for undiscovered hydrocarbons and to develop proven hydrocarbon reserves. However, the subject of subsurface mapping is probably the least discussed in Abu Dhabi, yet most important, aspect of petroleum exploration and development. This paper presents the tectonic map for Abu Dhabi based on gravity, magnetic and seismic interpretations, along with describing the various elements, their controlling faults and their effect on basin development and also rationalizes previously published structural and tectonic elements to clarify the kinematic relations and naming of individual tectonic elements. The method, which combines geologic, geophysical data in a comprehensive way, incorporates these data to simulate the interrelated effects of deposition and erosion of sediments and compaction, pressure, petroleum generation and multiphase fluid flow. The tectonic map of Abu Dhabi distinguishes three principal tectonic cycles: (1) Precambrian cycles are interpreted using the magnetic data, as there are no wells that penetrated the basement in Abu Dhabi and the seismic is mostly covering up to Jurassic layers. (2) The Paleozoic cycle began with continental rifting about 550 Ma, followed by inundation of much of Abu Dhabi by shallow seas. This cycle ended with the opening of the Neo-Tethys, which caused the deposition of the Mesozoic Cycle. (3) The Mesozoic cycle represents the legacy of ocean opening and the rise and fall of sea level created the stratigraphic and structural features that would later trap vast quantities of oil and gas. On the tectonic map, major features record this history. Abu Dhabi is affected by at least seven major tectonic events, which are shaping the present structures. However, these events can be complicated by the salt-movements (halokinesis) in offshore areas of Abu Dhabi, which resulted in change of structural relief and faults/fracture characterization particularly for deep reservoirs. Understanding of the kinematics and mechanics of the structures will highly impact the preservation of most of the hydrocarbons, and in turn reveals the new ventures to add reserves for Abu Dhabi.
机译:构造研究涉及地球外部的广泛建筑,年龄,关系,区域结构,变形和地壳特征的发展。地下地质地图也许是用于探索未被发现的碳氢化合物的最重要工具,并开发经过验证的碳氢化合物储备。然而,地下映射的主题可能是阿布扎比的最少讨论,但最重要的,最重要的,最重要的,大部分的石油勘探和发展方面。本文介绍了基于重力,磁性和地震解释的阿布扎比​​的构造图,以及描述了各种要素,控制故障及其对盆地发展的影响,也是为了阐明运动关系和命名的原始结构和构造元素。单个构造元素。将地质,地球物理数据以全面方式结合的方法包括这些数据,以模拟沉积和沉积,压力,石油产生和多相流体流动的相互关联的效果。阿布扎比的构造图区分了三个主要构造周期:(1)使用磁数据解释前亚洲周期,因为没有井穿过阿布扎比的地下室,地震大多覆盖到侏罗纪层。 (2)古生代周期开始于大陆渔罗约550 mA,随后在浅海中淹没了阿布扎比的大部分地区。该循环以新特质的开口结束,这导致了中生代周期的沉积。 (3)中生代周期代表海洋开放的遗产,海平面的上升和下降创造了后来捕获大量石油和天然气的地层和结构特征。在构造地图上,主要功能记录了这个历史。 Abu Dhabi受到至少七个主要构造事件的影响,这些事件正在塑造目前的结构。然而,这些事件可以在阿布扎比海上地区的盐运动(Halokinesis)复杂,这导致了结构浮雕和故障/骨折表征的变化,特别是对于深层储层。了解结构的运动学和力学将影响大多数碳氢化合物的保存,而且又揭示了新的企业为阿布扎比添加了储备。

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