Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Jean Dejou"'
Publikováno v:
CATENA. 56:21-30
The Belbex basalt is a Miocene alkaline basalt of the kind typical of the Massif Central of France and of continental rift systems generally. It outcrops as part of the Cantal stratovolcano in the vicinity of Aurillac. The current Cambisol overlies a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e0fd4cd653e173b0d5e6562b9d389596
https://doi.org/10.1016/j.catena.2003.10.018
https://doi.org/10.1016/j.catena.2003.10.018
Autor:
K. E. Bleich, H. Liedtke, Jean Dejou, Frank Ahnert, Ulrich Radtke, Dietrich Barsch, A. S. Goudie
Publikováno v:
Zeitschrift für Geomorphologie. 39:139-144
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15c678f9b1db955f08c6aecfe2f03d65
https://doi.org/10.1127/zfg/39/1995/139
https://doi.org/10.1127/zfg/39/1995/139
Autor:
Georges Baucher, Jean Dejou, Michel Lamand, François-Xavier Montard, Jacques Bellanger, Bernard Pons, Olivier Jourdan
Publikováno v:
Agronomie. 5:841-850
Un essai avec apport en couverture, pendant 3 annees consecutives, de Cu et de Zn sous forme de sulfates, a ete installe en sol volcanique de l'Auvergne. Cultive avec un ray-grass anglais, il a ete suivi pendant 8 ans avec plusieurs fertilisations di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c219ea10c60dc0a8fd0887208936ca85
https://doi.org/10.1051/agro:19850911
https://doi.org/10.1051/agro:19850911
Publikováno v:
Bulletin du Groupe français des argiles. 27:139-152
The diaclases of the granite massif with two micas of Crevant (Indre) are filled up by an argillaceous material with talc feel, very rich in fine-grained fractions, 70 % of clay particles being comprised between 0 and 20 µ. This material is composed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b94e397fbedd016a0eede34a9e73d334
https://doi.org/10.3406/argil.1975.1242
https://doi.org/10.3406/argil.1975.1242
Publikováno v:
Canadian Journal of Earth Sciences. 24:760-770
Samples were collected in a saprolite and soil profiles derived from the weathering of igneous pyroxenites at Mount Saint-Bruno, Quebec. Alternation of the disaggregated rock produces small amounts of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aceae40705c0f7d3332f77002be18615
https://doi.org/10.1139/e87-074
https://doi.org/10.1139/e87-074
Publikováno v:
Geochimica et Cosmochimica Acta. 45:1235-1243
A basalt and its weathered profile have been analysed for major elements. Graphical examination shows Al. Fe and Ti to have been essentially immobile. Determining mobility sequences for this deposit is complicated by the long pedogenetic history of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5102a83f067af72b5f63d2a77c57ff04
https://doi.org/10.1016/0016-7037(81)90147-2
https://doi.org/10.1016/0016-7037(81)90147-2
Autor:
Jean Dejou, Ward Chesworth
Publikováno v:
Soil Science. 130:290-292
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::553b7224601c9530991f9c3c4652a47d
https://doi.org/10.1097/00010694-198011000-00010
https://doi.org/10.1097/00010694-198011000-00010
Publikováno v:
Agronomie
Agronomie, EDP Sciences, 1984, 4 (1), pp.47-62
Agronomie 1 (4), 47-62. (1984)
Agronomie, EDP Sciences, 1984, 4 (1), pp.47-62
Agronomie 1 (4), 47-62. (1984)
Les Terres noires de Limagne rassemblent des sols qui, sur le plan génétique, sont à rattacher aux chernozems, aux brunizems et aux vertisols. L’étude de la composition minéralogique de la phase argileuse de ces différents sols révèle la pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f22066fd35b46efd8f369f7f7844cfaf
https://hal.science/hal-00884611
https://hal.science/hal-00884611
Publikováno v:
Périodiques Scientifiques en Édition Électronique.
Die geochemische Entwicklung der Diorite in der gemässigten Klimazone wurde an Hand von verschiedenen Profilen aus dem Limousin untersucht. Ebenso wie in den Graniten und den metamorphen Gesteinen besteht eine starke Grusbildung in den Dioritmassive
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9a4fea7570e35aa7f414855d3f70e53b
https://www.persee.fr/doc/sgeol_0302-2692_1972_num_25_4_1420
https://www.persee.fr/doc/sgeol_0302-2692_1972_num_25_4_1420