Multistage progressive evolution of rare osumilite-bearing assemblages preserved in ultrahigh-temperature granulites from In Ouzzal (Hoggar, Algeria)

Author:

Adjerid Z.12,Godard G.3,Ouzegane KH.2,Kienast J.-R.4

Affiliation:

1. Ecole Normale Supérieure Département des Sciences Naturelles; B.P. 92, Vieux Kouba Alger 16050 Algeria

2. Lab. de Géodynamique, Géologie de l'Ingénieur et de Planétologie; FSTGAT-U.S.T.H.B., B.P. 32 El Alia; Dar el Beida Alger 16111 Algeria

3. Institut de Physique du Globe; Sorbonne Paris Cité, Univ; Paris-Diderot, UMR 7154 CNRS; 1 rue Jussieu Paris Cedex 05 75238 France

4. Univ. Paris-Diderot; Paris 7 France

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Reference93 articles.

1. Kornerupine-quartz symplectites in paragneiss, Lac Ste-Marie, Quebec, Canada: pseudomorphic replacement of a hexagonal phase, probably osumilite;Ackermand;Mineralogy and Petrology,1999

2. First report of ultrahigh-temperature sapphirine + spinel + quartz and orthopyroxene + spinel + quartz parageneses discovered in Al-Mg granulites from the Khanfous area (In Ouzzal metacraton, Hoggar, Algeria). The Boundaries of the West African Craton;Adjerid;Geological Society, London, Special Publications,2008

3. Chronologie absolue du Précambrien de l'Ahaggar occidental;Allègre;Comptes rendus de l'Académie des Sciences, Paris,1972

4. Statistical control and optimization of X-ray intensity measurements;Ancey;Journal of Physics, D: Applied Physics,1977

5. Sillimanite and cordierite from volcanic xenoliths;Aramaki;American Mineralogist,1961

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