IODP
Expedition 301: The Hydrogeologic Architecture
of Basaltic Oceanic Crust: Compartmentalization, Anisotropy, Microbiology,
and Crustal-scale Properties on the Eastern Flank of Juan de Fuca Ridge |
Figure
5 |
(A) WST stacked waveforms and (B) determination of interval velocities for the 100-m section of open hole that was logged.
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