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The direction of fluid flow during contact metamorphism of siliceous carbonate rocks: New data for the Monzoni and Predazzo aureoles
Ist Teil von
Contributions to mineralogy and petrology, 2002-03, Vol.142 (6), p.679
Ort / Verlag
Heidelberg: Springer Nature B.V
Erscheinungsjahr
2002
Quelle
Alma/SFX Local Collection
Beschreibungen/Notizen
Periclase formed in siliceous dolomitic marbles during contact metamorphism in the Monzoni and Predazzo aureoles, the Dolomites, northern Italy, by infiltration of the carbonate rocks by chemically reactive, H2O-rich fluids at 500 bar and 565-710 degrees C. The new results for Monzoni and Predazzo are considered along with published studies of 13 other aureoles to draw general conclusions about the direction, amount, and controls on the geometry of reactive fluid flow during contact metamorphism of siliceous carbonate rocks.