Petrogenesis of LREE-rich pegmatitic granite dykes in the central Grenville Province by partial melting of Paleoproterozoic-Archean metasedimentary rocks: Evidence from zircon U-Pb-Hf-O isotope and trace element analyses-Reference-Cited by-同舟云学术

Petrogenesis of LREE-rich pegmatitic granite dykes in the central Grenville Province by partial melting of Paleoproterozoic-Archean metasedimentary rocks: Evidence from zircon U-Pb-Hf-O isotope and trace element analyses

Published:2019-07 Issue: Volume:327 Page:327-360
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Turlin François,Vanderhaeghe Olivier^ORCID,Gervais Félix,André-Mayer Anne-Sylvie,Moukhsil Abdelali^ORCID,Zeh Armin,Solgadi Fabien^ORCID,I.P.T.N.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference103 articles.

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3. A review of the relationships between granitoid types, their origins and their geodynamic environments;Barbarin;Lithos,1999

4. Residence of REE, Y, Th and U in Granites and Crustal Protoliths; Implications for the Chemistry of Crustal Melts;Bea;J. Petrology,1996

5. The growth of the continental crust: Constraints from zircon Hf-isotope data;Belousova;Lithos,2010

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