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Porosity and permeability images based on crosswell seismic measurements integrated with FMI logs at the Port Mayaca aquifer, South Florida

机译:基于井间地震测量和FMI测井的孔隙度和渗透率图像,位于南佛罗里达州马亚卡港含水层

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High-resolution seismic impedance delineated the upper confining unit contact intercepted by wells MF-37 and EXPM-1 at depths of 750 and 790 ft, respectively. This impedance image captures the variability of the soft and stiff zones in the interwell region. The impedance data with permeability and porosity well logs allow the generation of porosity and permeability images in the interwell region. These images visualize the flow units of high water production and low-rnpermeable zones or permeability barriers. On the other hand, FMI images provide information on the secondary porosity distribution at the borehole scale not detected with any other log. The sequences of conductive and resistive bands captured by the FMI images are in the stiff zones of the aquifer. The combined interpretation of FMI and crosswell images allows an improved understanding as to the origin of the high-permeability spikes developed near the well that are not significant conduits.
机译:高分辨率地震阻抗描绘了分别在750英尺和790英尺深度处被MF-37和EXPM-1井拦截的上部约束单元接触。该阻抗图像捕获井间区域中的软区和硬区的变化。具有渗透率和孔隙率测井曲线的阻抗数据允许在井间区域中生成孔隙率和渗透率图像。这些图像可视化了高产水量和低透水率区域或渗透屏障的流动单元。另一方面,FMI图像可提供有关井眼尺度的二次孔隙度分布的信息,而其他任何测井都无法检测到。 FMI图像捕获的导电带和电阻带的序列位于含水层的刚性区域中。 FMI和井间图像的组合解释可以更好地了解井附近形成的高渗透率尖峰的起源,这些尖峰不是重要的导管。

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