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Estimating vertical and horizontal resistivity of the overburden and the reservoir for the Alvheim - Boa field.

机译:估算覆盖层的垂直和水平电阻率和铝蟒蛇岩储层。

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Towed streamer EM data was acquired in October 2012 over the Alvheim - Boa Field located in the Norwegian sector of the North Sea. It is a challenging target consisting of a medium sized oil & gas field exhibiting an average transverse resistance located at 2,100 m below mudline. A depth model was defined for both the overburden and the reservoir interval based on an available well log, and the data was inverted as a series of 1D inversions for all common mid-points along two survey lines to form 2D resistivity sections. Both the vertical and horizontal resistivities were inverted for by minimizing the difference in the frequency responses between forward modeled data and the acquired towed streamer EM field data. Hence, the inversions were done with only a ten layer depth model as background information plus one value for the under-burden. The reservoir interval itself displays high anisotropy as expected since the reservoir is a turbidite. It consists of high resistivity hydrocarbon-charged sands inter-bedded with low resistivity shales giving rise to an effective anisotropy ratio of around 5, whereas the proximal overburden layer exhibits an anisotropy of 2.6. When the anisotropy can be evaluated, the net-to-gross can be estimated facilitating a much improved quantitative estimate of the hydrocarbons in place. Further, when an anisotropic reservoir is located in proximity to or directly on top of basement it can be detected by means of the anisotropy alone. The basement is likely to be isotropic or even display inverse anisotropy due to vertical fractures being more abundant, wider and hence also better conducting than tight horizontal fractures.
机译:位于北海挪威部门宝儿场 - 拖缆EM数据是在2012年10月在Alvheim收购。它是由一个中型油气田显示出位于在低于泥线2100米的平均横向阻力的一个具有挑战性的靶。深度模型两者上覆岩层和基于可用测井储层间隔来定义,并且数据被反转为一系列一维反转的用于沿两个测线所有常见的中点,以形成2D电阻率部分。垂直和水平电阻率进行了通过最小化前向建模的数据和所获取的拖缆EM场数据之间的频率响应的差反转。因此,反演单纯用十层深度模型为背景信息,以及为下一个负担值来完成。间隔本身储存器显示为预期的,因为贮存器是一个高浊各向异性。它由高电阻率的烃的带电砂的帧间层状具有低电阻率页岩引起的大约5的有效各向异性比,而近侧覆盖层显示出2.6的各向异性。当各向异性可以被评估,净毛比可估计促进烃代替显着改善的定量估计。另外,当各向异性水库位于接近或直接在基底的顶部上,可以通过单独的各向异性的装置检测。地下室很可能是各向同性的或甚至显示逆各向异性由于垂直裂缝是更丰富,更宽,因此也更好传导比紧水平裂缝。

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