Michel Campy
Datos Biográficos
| ID | 218644 |
|---|---|
| NOMBRE | Michel Campy |
| NOMBRES | Michel |
| APELLIDO | Campy |
| FIRMA | CAMPY M |
| AFILIACIONES | Centre National de la Recherche Scientifique |
| VERIFICADO | No |
| TOTAL DE OBRAS | 8 |
| TOTAL DE CITAS | 0 |
| OBRAS COMO AUTOR | 8 |
| OBRAS COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1989 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2014 |
| ÍNDICE H | 0 |
Frettes (Haute-Saône, France)
Late Pleistocene Detrital Sediment Yield of the Jura Glacier, France
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 the detrital material entering it from the Jura glacier accumulated. Sediment yield is computed from three factors: (1) the size of the sediment source area, (2) the length of time the system operated,…
Variations in Sediment Yield from the Upper Doubs River Carbonate Watershed (Jura, France) since the Late-Glacial Period
The Upper Doubs River Valley is a 910-km 2 watershed 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. The filling process and variations in sediment yield have been investigated by mechanical coring, seismic surveys, and electric soundings. The detrital sediment yield of the upstream watershed can …
Missing Records and Depositional Breaks in French Late Pleistocene Cave Sediments
Cave entrance and rock shelter infillings are positioned within the Pleistocene chronology for three areas of France (northern Alps, Franche-Comté, and Périgord). Despite minor local variations, it is possible to identify regional types with a consistent depositional record over long intervals of time. The interregional variability relates to the frequency and position of the gaps within the infillings. Sites in the northern Alps have not yielded…
La stratigraphie des dépôts
The filling of the porch of the Baume of Gigny is described level after level, from the top to the bottom of the stratigraphie series. Each individualized level is shown with its different lithologie characteristics, its thickness, its dip, its relationship with levels nearby, its lateral variations in fades
Étude sédimentologique du remplissage
L'étude sédimentologique du remplissage de La Baume de Gigny a été effectuée niveau par niveau. Les différents paramètres sédimentologiques sont définis et leur évolution étudiée de bas en haut de la séquence sédimentaire. L'évolution des différentes fractions granulométriques, la répartition des concrétions calcitiques et des galets allochtones, l'étude minéralogique et calcimétrique des fractions fines permettent d'interpréter les conditions de…
Chapitre I – Situation, cadre géologique et historique des fouilles
La grotte de La Baume à Gigny est située dans son contexte géographique et géologique. Site préhistorique reconnu dès la fin du XVIIIe siècle, les diverses recherches dont elle a été l'objet sont évoquées dans ce chapitre
Chapitre VI – La séquence chronoclimatique
The filling of the porch of the cave of the Baume in Gigny shows a stratigraphie sequence which spreads from the middle Pleistocene to present times. Five important chronoclimatic periods are clearly defined from biostratigraphic and sedimentological data, respectively : Suran stadial, Cressia interglacial, Gigny 1 stadial, Saint-Julien interstadial, Gigny 2 stadial, Loisia interstadial and Gigny 3 stadial. However, numerous gaps may be pointed o…
Sin obras prominentes en esta página.
La stratigraphie des dépôts
The filling of the porch of the Baume of Gigny is described level after level, from the top to the bottom of the stratigraphie series. Each individualized level is shown with its different lithologie characteristics, its thickness, its dip, its relationship with levels nearby, its lateral variations in fades
Étude sédimentologique du remplissage
L'étude sédimentologique du remplissage de La Baume de Gigny a été effectuée niveau par niveau. Les différents paramètres sédimentologiques sont définis et leur évolution étudiée de bas en haut de la séquence sédimentaire. L'évolution des différentes fractions granulométriques, la répartition des concrétions calcitiques et des galets allochtones, l'étude minéralogique et calcimétrique des fractions fines permettent d'interpréter les conditions de…
Chapitre I – Situation, cadre géologique et historique des fouilles
La grotte de La Baume à Gigny est située dans son contexte géographique et géologique. Site préhistorique reconnu dès la fin du XVIIIe siècle, les diverses recherches dont elle a été l'objet sont évoquées dans ce chapitre
Chapitre VI – La séquence chronoclimatique
The filling of the porch of the cave of the Baume in Gigny shows a stratigraphie sequence which spreads from the middle Pleistocene to present times. Five important chronoclimatic periods are clearly defined from biostratigraphic and sedimentological data, respectively : Suran stadial, Cressia interglacial, Gigny 1 stadial, Saint-Julien interstadial, Gigny 2 stadial, Loisia interstadial and Gigny 3 stadial. However, numerous gaps may be pointed o…
Missing Records and Depositional Breaks in French Late Pleistocene Cave Sediments
Cave entrance and rock shelter infillings are positioned within the Pleistocene chronology for three areas of France (northern Alps, Franche-Comté, and Périgord). Despite minor local variations, it is possible to identify regional types with a consistent depositional record over long intervals of time. The interregional variability relates to the frequency and position of the gaps within the infillings. Sites in the northern Alps have not yielded…
Variations in Sediment Yield from the Upper Doubs River Carbonate Watershed (Jura, France) since the Late-Glacial Period
The Upper Doubs River Valley is a 910-km 2 watershed 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. The filling process and variations in sediment yield have been investigated by mechanical coring, seismic surveys, and electric soundings. The detrital sediment yield of the upstream watershed can …
Late Pleistocene Detrital Sediment Yield of the Jura Glacier, France
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 the detrital material entering it from the Jura glacier accumulated. Sediment yield is computed from three factors: (1) the size of the sediment source area, (2) the length of time the system operated,…
Frettes (Haute-Saône, France)
Geography (5 obras) · Geology (5 obras) · Pleistocene-Era Hominins and Archaeology (5 obras) · Geology and Paleoclimatology Research (4 obras) · Paleontology (4 obras) · Archaeology (3 obras) · Geological formations and processes (3 obras) · Glacial period (3 obras) · Humanities (3 obras) · Physical geography (3 obras)