Zobrazeno 1 - 10
of 44
pro vyhledávání: '"Michel Campy"'
Autor:
Michel Campy
Cet ouvrage présente les différents cycles et les composantes interactives qui se déroulent à la surface des terres émergées : l'atmosphère et l'hydrosphère véhiculant matière et énergie, la lithosphère soumise à l'érosion et la biosph
Autor:
Michel Campy, Robert Arn
Publikováno v:
Boreas. 20:17-27
Since the first studies on the glacial formations of the Jura mountains there have been two concepts concerning type of glaciation and ice origin during the Wurmian glaciation. Some authors believed that the Jura was totally inundated by ice of Alpin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b8b5fb179822d98edd4205a6e2933ea0
https://doi.org/10.1111/j.1502-3885.1991.tb00455.x
https://doi.org/10.1111/j.1502-3885.1991.tb00455.x
Publikováno v:
Boreas
Boreas, Wiley, 1996, 25 (131-143), ⟨10.1111/j.1502-3885.1996.tb00841.x⟩
Boreas, 1996, 25 (131-143), ⟨10.1111/j.1502-3885.1996.tb00841.x⟩
Boreas, Wiley, 1996, 25 (131-143), ⟨10.1111/j.1502-3885.1996.tb00841.x⟩
Boreas, 1996, 25 (131-143), ⟨10.1111/j.1502-3885.1996.tb00841.x⟩
International audience; The changing palaeogeographical pattern of Alpine deposits across the European forelands can be traced by identifying mineral assemblages and establishing the chronology of Pliocene-Pleistocene deposits in Alpine foreland. In
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4f13446861817daa8d0a2a2065e5dbee
https://doi.org/10.1111/j.1502-3885.1996.tb00841.x
https://doi.org/10.1111/j.1502-3885.1996.tb00841.x
Autor:
Michel Campy, Jean-Jacques Macaire
Cet ouvrage présente les différents cycles et les composantes interactives qui se déroulent à la surface des terres émergées : l'atmosphère et l'hydrosphère véhiculant matière et énergie, la lithosphère soumise à l'érosion et la biosph
Autor:
Jean-Luc Deherripont, Gilles Huguenin, Michel Campy, Jean Detrey, Agnès Lamotte, Denis Morin, Hélène Corbeaux
Publikováno v:
L'anthropologie
L'anthropologie, Elsevier, 2014, 118 (4), pp. 449-475. 〈10.1016/j.anthro.2014.10.005〉
L'anthropologie, 2014, 118 (4), pp.449-475. ⟨10.1016/j.anthro.2014.10.005⟩
L'anthropologie, Elsevier Masson, 2014, 118 (4), pp.449-475. ⟨10.1016/j.anthro.2014.10.005⟩
L'anthropologie, Elsevier, 2014, 118 (4), pp. 449-475. 〈10.1016/j.anthro.2014.10.005〉
L'anthropologie, 2014, 118 (4), pp.449-475. ⟨10.1016/j.anthro.2014.10.005⟩
L'anthropologie, Elsevier Masson, 2014, 118 (4), pp.449-475. ⟨10.1016/j.anthro.2014.10.005⟩
International audience; Frettes is an open air site discovered in 1900 by Docteur Bouchet. Since that date, the site has been prospected by several other local researchers. The surface industry condensed by areas of 50 m2, shows something defined aro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0213c3c19fd60172324190c6379dfc91
https://hal.univ-lorraine.fr/hal-01491161
https://hal.univ-lorraine.fr/hal-01491161
Publikováno v:
Quaternary Research. 56:51-61
Measures of present-day glacial erosion vary widely with the technique employed. This paper quantifies the glacial material trapped in a proglacial lake during the Würm glacial period. The Combe d'Ain site was occupied by a meltwater lake where all
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31e7b873021a67746f254a7194fd10b0
https://doi.org/10.1006/qres.2001.2243
https://doi.org/10.1006/qres.2001.2243
Autor:
Michel Campy, Michel Meybeck, Christian Di-Giovanni, Hervé Richard, Vincent Bichet, Jean-François Buoncristiani
Publikováno v:
Quaternary Research. 51:267-279
The Upper Doubs River Valley is a 910-km2watershed feeding into Lake Chaillexon. The lake was formed by a natural rockfall at the end of the Bølling Chronozone (around 14,250 cal yr B.P.) and since then has trapped material eroded from the watershed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::22111797e74938fe9c5de20b1f4b03bd
https://doi.org/10.1006/qres.1999.2037
https://doi.org/10.1006/qres.1999.2037
Publikováno v:
Comptes Rendus de l'Acad�mie des Sciences - Series IIA - Earth and Planetary Science. 328:167-172
Matter fluxes result from chemical and mechanical weathering that vary as a function of climate, relief, lithology and human activities. The aim of this paper is to characterize chemical weathering variations in the past using coaly particles found i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d8560ea500be0f0b7cc4cba0200d0de3
https://doi.org/10.1016/s1251-8050(99)80092-5
https://doi.org/10.1016/s1251-8050(99)80092-5
Publikováno v:
Earth Surface Processes and Landforms. 23:1057-1069
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f3e88534345b748e50a3c49d494b0322
https://doi.org/10.1002/(sici)1096-9837(199812)23:12<1057::aid-esp921>3.0.co
https://doi.org/10.1002/(sici)1096-9837(199812)23:12<1057::aid-esp921>3.0.co
Publikováno v:
Earth Surface Processes and Landforms. 23:429-444
The middle valley of the river Ain (Jura) cuts through glacio-lacustrine deposits laid down in an ice-dammed lake during the most recent glacial advance. The total volume eroded is about 6·21 ×10 8 m 3 for a surface area of 3·7 ×10 7 m 2 . Erosio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f762800df05a1ea25346f8b5fa7f193a
https://doi.org/10.1002/(sici)1096-9837(199805)23:5<429::aid-esp858>3.0.co
https://doi.org/10.1002/(sici)1096-9837(199805)23:5<429::aid-esp858>3.0.co