A study of a natural system concerning the growth of minerals (garnet) into metapelite host rocks from Calabria (southern Italy), which underwent pressure up to 1.2 GPa, is presented. Through the application of a thermodynamic model it was possible to determine P and T conditions achieved during metamorphic evolution of these rocks useful to reconstruct the related tectonic settings of poly-orogenic metamorphic complexes.
Titolo: | Garnet growth in natural high pressure regime: a key tool in unravelling the pressure-temperature path of rocks involved in mountain belt orogeny |
Autori interni: | |
Data di pubblicazione: | 2008 |
Rivista: | |
Handle: | http://hdl.handle.net/20.500.11769/6356 |
Appare nelle tipologie: | 1.1 Articolo in rivista |
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