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Fig 9 - Halogens in Seawater, Marine Sediments and the Altered Oceanic Lithosphere

Fig. 9.5 Schematic diagram highlighting the slab bend as an important site for deep (>20 km) fractures and hydrothermal alteration of the lithospheric mantle (see text). Note that fractures at the slab bend provide a possible pathway for sedimentary pore waters to infiltrate the lithosphere 
5 Schematic diagram highlighting the slab bend as an important site for deep (>20 km) fractures and hydrothermal alteration of the lithospheric mantle (see text). Note that fractures at the slab bend provide a possible pathway for sedimentary pore waters to infiltrate the lithosphere 
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