Squirt flow due to interfacial water films in hydrate bearing sediments
Sediments containing gas hydrate dispersed in the pore space are known to show a characteristic seismic anomaly which is a high attenuation along with increasing seismic velocities. Currently, this observation cannot be fully explained albeit squirt-flow type mechanisms on the microscale have be...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2018-05-01
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| Series: | Solid Earth |
| Online Access: | https://www.solid-earth.net/9/699/2018/se-9-699-2018.pdf |