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Ultrahigh Pressure Metamorphism (UHPM) is a fast growing discipline
that was established 25 years ago after discoveries of high
pressure minerals, coesite and diamonds. The current explosion of
research on UHMP terranes reflects their significance for
understanding large scale mantle dynamics, major elements of plate
tectonics such as continental collisions, deep subduction and
exhumation, mountains building, geochemical recycling 'from surface
to the core', and a deep storage of light elements participating in
green-house effects in the atmosphere. This book provides insights
into the formation of diamond and coesite at very high pressures
and explores new ideas regarding the tectonic setting of this style
of metamorphism.
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