Figure F16. Profile of the lithium (Li+) to chloride (Cl-) concentration (molar x 10-4) ratio at Site 1244 compared to the distribution reported for Site 888, which was drilled west of the deformation zone during ODP Leg 146 (Westbrook, Carson, Musgrave, et al., 1994; Kastner et al., 1995). The similarity between these distributions suggests a common source of fluids deep within the accreted sediments of the Cascadia prism.

Figure F16. Profile of the lithium (Li⁺) to chloride (Cl^-) concentration (molar x 10^-4) ratio at Site 1244 compared to the distribution reported for Site 888, which was drilled west of the deformation zone during ODP Leg 146 (Westbrook, Carson, Musgrave, et al., 1994; Kastner et al., 1995). The similarity between these distributions suggests a common source of fluids deep within the accreted sediments of the Cascadia prism.