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Seismic imaging of a thin unconventional reservoir in highly attenuating media: the case of the Macasty Formation, Anticosti Island, Canada

机译:高衰减媒体中薄的非传统水库的地震成像:加拿大北京天空岛的修道院形成的情况

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Seismic wave propagation through the subsurface is characterized by a loss of high frequency energy desired for high-resolution imaging at depth. This means that the size of geological features that can be resolved increases with depth. In this context, exploration of thin-layered unconventional reservoirs represents a significant challenge for seismic imaging. Here the case of the Macasty Formation, a thin-layered shale reservoir included in a highly attenuating limestone-dominated Silurian-Ordovician succession, is discussed. To retrieve high frequency energy, Q-phase compensation, zero-phase deconvolution and a 90°-phase rotation followed by the application of a Butterworth filter are used. Results provide an amplitude spectrum that is flatter and broader compared to the original data. New imaging resolves internal high amplitude reflections within the reservoir that are correlative to higher TOC values of the pay-zone.
机译:通过地下的地震波传播的特征在于,在深度的高分辨率成像期望的高频能量的损失。 这意味着可以解决的地质特征的大小随深度而增加。 在这种情况下,薄层非传统水库的探索是地震成像的重大挑战。 在这里,讨论了修道院形成的薄层页岩水库,包括在高度衰减的石灰石主导的Silurian-Ordovician连续继承中。 为了检索高频能量,q相补偿,零相块卷积和90°相旋转,然后使用施加Butterworth滤波器。 结果提供了与原始数据相比更平坦和更广泛的幅度频谱。 新的成像解析了储层内的内部高幅度反射,这些反射是与工资区的更高TOC值相关的相关性。

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