Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Michel Icole"'
Publikováno v:
Journal of African Earth Sciences. 26:249-259
Resume La lagune de Nador, en bordure de la Mediterranee, est situee a l'extremite Est du Rif oriental marocain. Les depots superficiels montrent trois facies: sableux, argilo-silteux et argilo-silto-sableux. Les corteges de mineraux argileux sont pe
Autor:
Sigfus J Johnsen, David Williamson, Jean Jouzel, Joel Guiot, Trevor Williams, Maurice Reille, Nicolas Thouveny, K.M. Creer, Jacques-Louis de Beaulieu, Eugène Bonifay, Michel Icole
Publikováno v:
Nature
Nature, Nature Publishing Group, 1994, 371 (6497), pp.503-506. ⟨10.1038/371503a0⟩
Nature, 1994, 371 (6497), pp.503-506. ⟨10.1038/371503a0⟩
Nature, Nature Publishing Group, 1994, 371 (6497), pp.503-506. ⟨10.1038/371503a0⟩
Nature, 1994, 371 (6497), pp.503-506. ⟨10.1038/371503a0⟩
International audience; RAPID shifts in climate during the last glacial are now well documented, particularly from the oxygen isotope records of the two Greenland ice cores GRIP(1,2) and GISP2(3). In the GRIP record(1,2) these climate events are also
Publikováno v:
Global and Planetary Change. 7:235-242
Magnetic parameters measurements (magnetic susceptibility χ and Isothermal Remanent Magnetizations (IRMs) and sedimentological analyses have been performed on Late Pleistocene/Holocene laminated deposits from Lakes Natron and Magadi (Kenya). Acceler
Autor:
Maurice Taieb, Michel Icole, Philip A. Barker, Brahlm Damnati, David Williamson, Nell Roberts
Publikováno v:
Nature. 366:146-148
THE last deglaciation was interrupted by an abrupt cooling event, the Younger Dryas, at 11,000& ndash;10,000 yr BP (uncalibrated radiocarbon timescale)1. Originally recognized in climate records from northwest Europe, the Younger Dryas has now been i
Publikováno v:
Bulletin de la Société Géologique de France. :1305-1318
Publikováno v:
Sciences Géologiques. Bulletin. 40:71-82
Sedimentary units of the Peninj Group located at the western edge of Lake Natron (Tanzania) include the Humbu and the Moinik formations. Their age is between approximately 1.6 and 1.0 Ma. The Humbu Formation is consisting of lacustrine deposits with
Publikováno v:
Bulletin de l'Association française pour l'étude du quaternaire. 21:60-66
Soils and particularly weathering rocks data on alluvial gravels tends to assumption of a non-synchronism for alluvial setting between upper and lower part of the basin. With regard to a lower terrace so called « basse plaine », this assumption is
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 42:273-284
Sodium silicates and chert of similar appearance are often considered as environmental indicators: saline playas with shallow ground-water tables for magadiite, kanemite and makatite formation; post-evaporite environment for kenyaite and chert by lea
Autor:
Michel Icole
Publikováno v:
Bulletin de l'Association française pour l'étude du quaternaire. 7:135-143
It is shown that each weathered corona surrounded quartzite pebbles and some characteristics of the matrix can be regarded as the result of the same pedogenesis. Consequently each individualized pedological evolution, can be jointly studied on the ma
Publikováno v:
Périodiques Scientifiques en Édition Électronique.
In the Manga, of Niger (North-West of Lake Chad), the depressions between dunes have kept the mark of water table fluctuation related to climate. The succession of events is : sedimentation of diatomite, nodulation of concretions of sodium silicates,