The scientists were now able to observe the formation of a new phase of the mineral, so - called
super-hydrated kaolinite.
The observation of the formation and breakdown of
the super-hydrated kaolinite bears important information about the processes that occur over a depth range of about 75 kilometres to 480 kilometres in subduction zones.
Additionally,
the super-hydrated kaolinite could influence seismicity.
The release of water that takes place when
the super-hydrated kaolinite breaks down could be an important part of the water cycle that causes volcanism along subduction zones.
Not exact matches
The first observation of a
super-hydrated phase of the clay mineral
kaolinite could improve our understanding of processes that lead to volcanism and affect earthquakes.