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f Seismic attenuation in thinly layered, fluid saturated and permeable sediments
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, 58th EAGE Conference and Exhibition, Jun 1996, cp-48-00059
- ISBN: 978-90-73781-07-8
Abstract
Typical reservoir rocks are often thinly layered, porous, fluid saturated and permeable sediments. Scattering of an incident wavefield by thin layering is an important reason for the attenuation of seismic waves in sediments.