Figure F13. Distribution of dissolved chloride and lithium in pore waters from Holes 1251B and 1251C. The increase in lithium and decrease in chloride with depth suggest a fluid source within the deep-seated sediments of the accretionary complex.

Figure F13. Distribution of dissolved chloride and lithium in pore waters from Holes 1251B and 1251C. The increase in lithium and decrease in chloride with depth suggest a fluid source within the deep-seated sediments of the accretionary complex.