Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Jean-Michel Puig"'
Autor:
Gérard Sauzade, Jacques Buisson-Catil, Alain Couturaud, Jean-Michel Puig, Anne Hasler, Stéphanie Thiébault
Publikováno v:
Documents d'Archéologie Méridionale. 19:1-98
Thiébault Stéphanie, Sauzade Gérard, Buisson-Catil Jacques, Hasler Anne, Puig Jean-Michel, Couturaud Alain. Le gisement Bronze final de l'aven des Fourches I à Sault. Contribution à l'étude fonctionnelle des cavités karstiques des plateaux de
Publikováno v:
Environmental Geology and Water Sciences. 19:215-225
The intake area of the Fontaine de Vauctuse system covers over 1,100 km2; its mean altitude is 870 m. The Lower Cretaceous limestones (1,500 m thick) give the system a very thick (800 m) unsaturated zone. Karstification is very well developed, both o
Publikováno v:
Geodinamica Acta. 5:153-172
ResumenL’aquifere karstique de la celebre Fontaine de Vaucluse a fait l’objet de nouvelles investigations hydrogeologiqurs dont les resultats portent sur la definition et le fonctionnement du systeme.Les donnees geologiques (lithologie, structure
Autor:
Martial Dray, Gian Maria Zuppi, F. Pollicini, Gabriel de los Cobos, Jean-Paul Novel, Gérard Nicoud, F. Bonetto, Serge Fudral, Aurèle Parriaux, André Paillet, Philippe Olive, Jean-Michel Puig
Publikováno v:
Périodiques Scientifiques en Édition Électronique.
L'attuale morfologia dovuta a fenomeni e depositi gravitativi, torrentizi ed alluvionali, nasconde una potente successione sedimentaria legata ad una dinamica lacustre evolutasi in due fasi : -la formazione di un primo lago, maggiore per dimensioni e
Publikováno v:
Geophysical Research Letters
Geophysical Research Letters, American Geophysical Union, 1998, 25 (9), pp.1459-1462. ⟨10.1029/98GL01056⟩
Geophysical Research Letters, American Geophysical Union, 1998, 25 (9), pp.1459-1462. ⟨10.1029/98GL01056⟩
International audience; This work aims at using the Dissolved Organic Carbon (DOC) as a tracer of infiltration in karstic aquifers with only diffuse recharge. Regular measurements of DOC have been carried out in three karstic systems located in South
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::718623ebd915f7b2f73c9e7d70eaa1f6
https://hal-univ-avignon.archives-ouvertes.fr/hal-02296885/document
https://hal-univ-avignon.archives-ouvertes.fr/hal-02296885/document
Publikováno v:
Comptes Rendus de l'Académie des Sciences-Series IIA-Earth and Planetary Science
Comptes Rendus de l'Académie des Sciences-Series IIA-Earth and Planetary Science, Elsevier, 1998, 326 (5), pp.327-332. ⟨10.1016/S1251-8050(98)80302-9⟩
Comptes Rendus de l'Académie des Sciences-Series IIA-Earth and Planetary Science, Elsevier, 1998, 326 (5), pp.327-332. ⟨10.1016/S1251-8050(98)80302-9⟩
International audience; By using 13C as a tracer in karstic aquifers, one can distinguish between water from the unsaturated and the saturated zones, because the system behaves as one open to the biogenic CO2 in the unsaturated zone. This method show
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f4f6cd6d4feb6d012262ce7afd19beb5
https://hal-univ-avignon.archives-ouvertes.fr/hal-02296833
https://hal-univ-avignon.archives-ouvertes.fr/hal-02296833
Autor:
Alain Couturaud, Jacques Buisson-Catil, Gérard Sauzade, Jean-Michel Puig, Stéphanie Thiébault, Anne Hasler
Publikováno v:
Documents d'archéologie méridionale
Documents d'archéologie méridionale, 1996, 19, pp.7-31. ⟨10.3406/dam.1996.1164⟩
Documents d'archéologie méridionale, 1996, 19, pp.7-31. ⟨10.3406/dam.1996.1164⟩
The excavation of a karstic cavity (aven), hollowed out in the Vaucluse plateaux, led to the discovery of numerous remains (mainly pottery) from the Late Neolithic and particularly from the Late Bronze Age (LB 1 and LB 2). Although a true stratigraph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1b79782169b2d9439d82cf5d850b11e9
https://hal.science/hal-03829475
https://hal.science/hal-03829475
Autor:
Jean-Michel Puig, Alain Couturaud
Publikováno v:
Périodiques Scientifiques en Édition Électronique.
A double tracing was carried out in 1989 at the edge of the large karst system of the Vaucluse : 25 kg of fluorescein were poured into the trou du Vent, 1335 m up on the north side of mont Ventoux and 20 kg of sulforhodamin into the sinkhole of a str
Autor:
Jacques Mudry, Jean-Michel Puig
Publikováno v:
Périodiques Scientifiques en Édition Électronique.
The intake area of the Fontaine de Vaucluse system is more than 1100 km2 wide, with an average altitude of 870 m. The thickness of the lower cretaceous limestones (1500 m) gives the system a very thick (800 m) unsatura¬ ted zone. Karstification is h