Abstract
Abstract Granitic rocks represent a ubiquitous component of upper continental crust but their origin remains highly controversial. This controversy stems from the fact that the granites may result from fractionation of mantle-derived basaltic magmas or partial melting of different crustal protoliths at contrasting pressure–temperature conditions, either water-fluxed or fluid-absent. Consequently, many different mechanisms have been proposed to explain the compositional variability of granites ranging from whole igneous suites down to mineral scale. This Special Publication presents an overview of the state of the art and envisages future avenues towards a better understanding of granite petrogenesis.
Highlights
Granite represents a ubiquitous rock type dominating the upper–middle continental crust (Taylor & McLennan 2009; Rudnick & Gao 2014)
Granitic rocks represent a ubiquitous component of upper continental crust but their origin remains highly controversial
This controversy stems from the fact that the granites may result from fractionation of mantle-derived basaltic magmas or partial melting of different crustal protoliths at contrasting pressure–temperature conditions, either water-fluxed or fluid-absent
Summary
Granite (sensu lato) represents a ubiquitous rock type dominating the upper–middle continental crust (Taylor & McLennan 2009; Rudnick & Gao 2014). This controversy stems from the fact that the granites may result from fractionation of mantle-derived basaltic magmas or partial melting of different crustal protoliths at contrasting pressure–temperature conditions, either water-fluxed or fluid-absent.
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