Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Michel Gravelle"'
Autor:
Michel Villeneuve, Pierre Saint-Marc, Michel Gravelle, Hervé Bellon, Christian Honthaas, Jean-Jacques Cornée, Safri Burhanuddin, Jacques Butterlin, Jean-Pierre Réhault
Publikováno v:
Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science. 325:883-890
Resume De nouvelles donnees biostratigraphiques, geochronologiques et geochimiques sur l'ile de Kur et deux dragages adjacents permettent de montrer l'existence d'evenements auparavant inconnus sur la marge est du bassin de Weber : le fonctionnement
Publikováno v:
Bulletin de la Société Géologique de France. :677-684
Publikováno v:
Bulletin de la Société Géologique de France. :43-54
Autor:
Michel Gravelle
Publikováno v:
Bulletin de la Société Géologique de France. :218-222
In the region of Silet (western Ahaggar, central Sahara) two major volcanic episodes predating the deposition of the Cambro-Ordovician Tassilis sandstone are identified. They are definitely pre-Tremadoc (uppermost Cambrian or lowermost Ordovician) an
Autor:
M. Lelubre, Michel Gravelle
Publikováno v:
Bulletin de la Société Géologique de France. :435-442
Stromatolites belonging to the Conophyton group are described from Pharusian (Precambrian) marbles of the western Ahaggar region (Algeria) in the central Sahara, and compared with closely related forms from the western Sahara. They represent the olde
Autor:
Michel Gravelle
Publikováno v:
Bulletin de la Société Géologique de France. :143-151
Poorly fossiliferous detrital and volcanic beds of the so-called "intermediate series" outcrop in the eastern part of the Pharusian (Precambrian) trough in the western Ahaggar mountains and on the western border of the Suggarian (Precambrian) horst o
Autor:
Michel Gravelle
Publikováno v:
Bulletin de la Société Géologique de France. :336-339
The Pharusian (Precambrian) conglomerates associated with the I-n-Temeroueline complex have been discovered on the northwestern side of the I-n-Temerouelt hills, thus extending the known limit of the Pharusian trough considerably to the west.