If the fault zone does not have
hydrous phases or carbonates, the sudden heating that begins when sliding starts raises the local temperature on the fault all the way to the melting temperature of the rock.
«The reason this does not happen often, that is, the reason we do not see lots of faults with glass on them, is that the Earth's crust is made up to a large degree of
hydrous and carbonate
phases, and even the rocks that don't have such
phases usually have feldspars that get crushed up in the fault zone,» Green explained.