Intracratonic asthenosphere upwelling and lithosphere rejuvenation beneath the Hoggar swell (Algeria): Evidence from HIMU metasomatised lherzolite mantle xenoliths

Author:

Beccaluva L.,Azzouni-Sekkal A.,Benhallou A.,Bianchini G.,Ellam R.M.,Marzola M.,Siena F.,Stuart F.M.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference57 articles.

1. Nouvelles données géochronologiques et isotopiques sur le volcanisme cénozoïque de l'Ahaggar (Sahara algérien): des arguments en faveur d'un panache;Aït-Hamou;Comptes Rendus de l'Académie des Sciences de Paris,2000

2. The sub-continental versus sub-oceanic debate. Lead–neodymium–strontium isotopes in primary basalts in a shield area: the Ahaggar volcanic suite;Allègre;Earth Planet. Sci. Lett.,1981

3. Crustal and upper mantle velocity structure of the Hoggar swell (Central Sahara, Algeria);Ayadi;Phys. Earth Planet. Inter.,2000

4. Tertiary alkaline volcanism of the Atakor Massif (Hoggar, Algeria);Azzouni-Sekkal,2007

5. Nephelinitic to tholeiitic magma generation in a transtensional tectonic setting: an integrated model for the Iblean volcanism, Sicily;Beccaluva;J. Petrol.,1998

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