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 2


Two-way travel time seismic reflection profile showing the location of Site U1301 that was drilled during IODP Expedition 301 (Expedition 301 Preliminary Report, 2004). This seismic data was acquired with the 2000 ImageFlux survey (Sonne, SO149). Vertical lines on this figure represent approximate total depth of Holes U1301A (shallower hole) and U1301B (deeper hole).