SEG Technical Program Expanded Abstracts 2012 2012
DOI: 10.1190/segam2012-0508.1
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Velocity Modeling to Determine Pore Aspect Ratios of the Haynesville Shale

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“…This leads to a higher seismic velocity than that obtained with interparticle pores. In contrast, thin or elongated pores such as cracks and microporosity often lead to slower velocity by rock softening (Oh and Spikes, 2012). The pore aspect ratio is a textural parameter that contributes for stiffness or softness carbonate rock characterization.…”
Section: Introductionmentioning
confidence: 98%
“…This leads to a higher seismic velocity than that obtained with interparticle pores. In contrast, thin or elongated pores such as cracks and microporosity often lead to slower velocity by rock softening (Oh and Spikes, 2012). The pore aspect ratio is a textural parameter that contributes for stiffness or softness carbonate rock characterization.…”
Section: Introductionmentioning
confidence: 98%