K, Rb, Sr, Ba, U and Th geochemistry of the Lapland Granulites (Fennoscandia). LILE fractionation controlling factors

Author:

Barbey P.,Cuney M.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference66 articles.

1. Allen AR (1979) Metasomatism of a depleted granulite facies terrain in the Arunta Block, Central Australia. Contrib Mineral Petrol 71:85?98

2. Barbey P (1982) Signification géodynamique des domaines granulitiques. La ceinture des granulites de Laponie (Fennoscandie): une suture de collision continentale d'âge Protérozoïque inférieur (2.3-1.9 Ga). Reconstitution pétrologique et géochimique. Unpubl Thesis, Nancy, 1?346

3. Barbey P, Convert J, Moreau B, Martin H, Capdevila R, Hameurt J (1980) Relationships between granite ? gneiss terrains, greenstone belts and granulite belt in the Archean crust of Lapland (Fennoscandia). Geol Rundsch 69:648?658

4. Barbey P, Capdevila R, Hameurt J (1982) Major and transition trace element abundances in the khondalite suite of the granulite belt of Lapland (Fennoscandia): evidence for an early Proterozoïc flysch-belt. Precambrian Research 16:273?290

5. Bernard-Griffiths J, Vidal Ph, Peucat JJ Isotopic ages (U-Pb, Rb-Sr, Sm-Nd) of mafic metaigneous granulites from the granulite belt of Finnish Lapland (to appear)

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