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From granulite fluids to quartz-carbonate megashear zones: The gold rush

Fu, Bin; Touret, Jacques L.R.


At peak granulite-facies metamorphic conditions, lower continental crust is arguably fluxed by large amounts of two key low water activity fluids: (i) high-density CO2 and/or (ii) concentrated saline solutions. These fluids are either internally-derived,

CollectionsANU Research Publications
Date published: 2014
Type: Journal article
Source: Geoscience Frontiers (Previously Earth Science Frontiers)
DOI: 10.1016/j.gsf.2014.03.013


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