(Table 1) Bulk and grain density, porosity, and p- and s-wave velocity characteristics of ODP Hole 163-990A sediments
Seismic velocities in rocks are influenced by the properties of the solid, the pore fluid, and the pore space. Cracks dramatically affect seismic velocities in rocks; their influence on the effective elastic moduli of rocks depends on their shape and concentration. Thin cracks (or fractures) substan...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1999
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.804640 https://doi.org/10.1594/PANGAEA.804640 |