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Crosswell seismic imaging of acoustic and shear impedance in a Michigan reef

机译:密歇根州礁石的声学和剪切阻抗的Crosswell地震成像

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Crosswell seismic imaging has demonstrated its ability to provide extremely high-quality images of reservoirs such that internal features within the reef can be imaged and character-rnized. Resolution is about 40 times that of surface seismic in the same area (50 Hz versus 2000 Hz).rnThe amplitudes of reflectors from within the Springdale reef are low, however, and especially so for the image obtained from above. We attribute this to attenuation and scattering of signal as it passes through the complex upper part of the reef, where gas saturation likely varies locally, reservoir pressure is extremely low, and structural complexity of the reef is evident. The image from beneath does not pass through this complexity and only experiences the gas saturation and low pressures at the upper edge of the image, allowing most of the image to be higher quality.
机译:克罗斯韦尔地震成像技术已经证明其能够提供极高质量的储层图像,从而可以对礁石内部特征进行成像和特征化。分辨率大约是同一地区(50 Hz对2000 Hz)的地表地震的40倍。rn但是,斯普林代尔礁内的反射器振幅很低,尤其是从上方获得的图像。我们将其归因于信号穿过礁石的复杂上部时的衰减和散射,其中气体饱和度可能会局部变化,储层压力极低,并且礁石的结构复杂性显而易见。下方的图像不会经历这种复杂性,仅会在图像的上边缘经历气体饱和度和低压,从而使大多数图像具有更高的质量。

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