Stability of Al- and F-rich titanite in metacarbonate: petrologic and isotopic constraints from a polymetamorphic eclogitic marble of the internal Sesia Zone (Western Alps)
Al- and F-rich titanite (3.86< Al2O3 < 9.33 wt%, 0.93< F < 2.53 wt%) from a polymetamorphic marble of the Sesia Zone (Western Alps) has been investigated in order to determine the behaviour of titanite during high-pressure metamorphism. Meso-structural to micro-structural relationships, mineral assemblages and petrological data indicate a pre-Alpine (low-pressure, high-temperature) to early-Alpine (high-pressure, medium-temperature) pressure-temperature-time evolution. Backscattered electron...[Show more]
|Collections||ANU Research Publications|
|Source:||Contributions to Mineralogy and Petrology|
|01_Castelli_Stability_of_Al-_and_F-rich_2002.pdf||444.02 kB||Adobe PDF||Request a copy|
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