Articles | Volume 36, issue 1
https://doi.org/10.5194/ejm-36-225-2024
https://doi.org/10.5194/ejm-36-225-2024
Research article
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21 Feb 2024
Research article | Highlight paper |  | 21 Feb 2024

Granite magmatism and mantle filiation

Michel Pichavant, Arnaud Villaros, Julie A.-S. Michaud, and Bruno Scaillet

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Cited articles

Albarède, F., Dupuis, C., and Taylor Jr., H. P.: 18O/16O evidence for non-cogenetic magmas associated in a 300 Ma old concentric pluton at Ploumanac'h (Brittany, France), J. Geol. Soc. Lond., 137, 641–647, 1980. 
Annen, C., Blundy, J. D., and Sparks, R. S. J.: The genesis of intermediate and silicic magmas in deep crustal hot zones, J. Petrol., 47, 505–539, 2006. 
Annen, C., Blundy, J. D., Leuthold, J., and Sparks, R. S. J.: Construction and evolution of igneous bodies: towards an integrated perspective of crustal magmatism, Lithos, 230, 206–221, 2015. 
Aranovich, L. Y., Newton, R. C., and Manning, C. E.: Brine-assisted anatexis: experimental melting in the system haplogranite–H2O–NaCl–KCl at deep-crustal conditions, Earth Planet. Sc. Lett., 374, 111–120, 2013. 
Aranovich, L. Y., Makhluf, A. R., Manning, C. E., and Newton, R. C.: Dehydration melting and the relationship between granites and granulites, Precambrian Res., 253, 26–37, 2014. 
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Short summary
Models for the generation of silicic magmas are divided into two groups: intra-crustal melting and basaltic origin. Peraluminous felsic leucogranites are considered as the only granite examples showing no mantle input. This interpretation is re-evaluated, and we show that leucogranites, as most other crustal granite types, can have a mantle filiation. This stresses the critical importance of the mantle for granite generation and opens the way for unification of silicic magma generation models.