Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Pierre A. Cousineau"'
Autor:
Jean-François Ghienne, Etienne Brouard, Pierre A. Cousineau, Alexis Nutz, Patrick Lajeunesse, Mathieu Schuster, Claude Roquin, Frédéric Bouchette, Pierre Dietrich
Publikováno v:
Nutz, A, Lajeunesse, P, Ghienne, J F, Schuster, M, Brouard, E, Dietrich, P, Bouchette, F, Roquin, C & Cousineau, P A 2020, Deglacial to Paraglacial History of the Lake Saint-Jean Lowlands : A Geomorphological Perspective . in O Slaymaker & N Catto (eds), Landscapes and Landforms of Eastern Canada . Springer, Cham, World Geomorphological Landscapes, pp. 145-158 . https://doi.org/10.1007/978-3-030-35137-3_5
World Geomorphological Landscapes ISBN: 9783030351359
Landscapes and Landforms of Eastern Canada
Olav Slaymaker & Norm Catto (Eds.). Landscapes and Landforms of Eastern Canada, Springer, pp.145-158, 2020, World Geomorphological Landscapes book series (WGLC), 978-3-030-35135-9. ⟨10.1007/978-3-030-35137-3_5⟩
World Geomorphological Landscapes ISBN: 9783030351359
Landscapes and Landforms of Eastern Canada
Olav Slaymaker & Norm Catto (Eds.). Landscapes and Landforms of Eastern Canada, Springer, pp.145-158, 2020, World Geomorphological Landscapes book series (WGLC), 978-3-030-35135-9. ⟨10.1007/978-3-030-35137-3_5⟩
International audience; The Lake Saint-Jean lowland is a particular area in eastern Canada as it constitutes an important Late Quaternary depocenter compared with other surrounding onshore regions. Here, the recent literature about the Late Quaternar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::82a8f56ae5dc5e94701b384059c178e8
https://pure.au.dk/portal/da/publications/deglacial-to-paraglacial-history-of-the-lake-saintjean-lowlands(45bad3b3-83cf-4426-b305-e419274c6432).html
https://pure.au.dk/portal/da/publications/deglacial-to-paraglacial-history-of-the-lake-saintjean-lowlands(45bad3b3-83cf-4426-b305-e419274c6432).html
Publikováno v:
Boreas. 45:754-772
The Charlevoix region, in southeastern Quebec, is characterized by a dramatic landscape formed by the junction of the Laurentian Highlands, the Charlevoix Astrobleme and the St Lawrence Estuary. At the Last Glacial Maximum (LGM), the region was compl
Publikováno v:
Journal of Sedimentary Research. 86:542-563
Conventional provenance studies of high grade (e.g., amphibolite facies) metamorphic sandstone are limited due to intense recrystallization, destruction of original minerals, and growth of new minerals. Magnetite is a heavy mineral common in a wide r
Autor:
Pierre A. Cousineau, P. T. Simard, Mélanie Lambert, Réal Daigneault, Brigitte Poirier, Léo Poignant-Molina, Denis W. Roy, Alain Rouleau, Romain Chesnaux
Publikováno v:
Journal of Applied Geophysics. 119:36-50
Aquifer formations along the northern shore of the Saint-Lawrence River in Quebec (Canada) mainly consist of glacial and coastal deposits of variable thickness overlying Precambrian bedrock. These deposits are important because they provide the main
Publikováno v:
Environmental Earth Sciences. 74:4671-4683
The construction of 3D hydrogeological models for unconsolidated sedimentary aquifers remains particularly challenging, especially in Quaternary deposits. Simplifications at small or large scale are part of groundwater flow modeling and are often req
Autor:
Frédéric Bouchette, Pierre A. Cousineau, Raphaël Certain, Claude Roquin, Jean-François Ghienne, Olivier Raynal, Alexis Nutz, Philippe Duringer, Nicolas Robin, Mathieu Schuster
Publikováno v:
Boreas. 43:309-329
The stratigraphy of the last deglaciation sequence is investigated in Lake Saint-Jean (Quebec Province, Canada) based on 300 km of echo-sounder two dimensional seismic profiles. The sedimentary archive of this basin is documented from the Late Pleist
Autor:
Pierre A. Cousineau, Alexis Nutz, Murray B. Hay, Claude Roquin, Mathieu Schuster, Pierre Dietrich, Jean-François Ghienne, Frédéric Bouchette
Publikováno v:
Sedimentology
Sedimentology, Blackwell Publishing, 2015, 38p. ⟨10.1111/sed.12196⟩
Sedimentology, Blackwell Publishing, 2015, 38p. ⟨10.1111/sed.12196⟩
Differentiating between forced regressive deposits from deglacial periods in high latitude domains and forced regressive deposits from the onset of glacial periods in low latitude domains is fundamental for the accurate interpretation of glacial cycl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3cc6258ad3678bdd48d63de021a52b1d
https://hal-insu.archives-ouvertes.fr/insu-01184731
https://hal-insu.archives-ouvertes.fr/insu-01184731
Autor:
Olivier Raynal, Sirocco Team, Frédéric Bouchette, Fabien Retif, Murray B. Hay, Alexis Nutz, Claude Roquin, M. Schuster, Nicolas Robin, Jean-François Ghienne, Raphaël Certain, Pierre A. Cousineau
Publikováno v:
Geological Society of America Bulletin
Geological Society of America Bulletin, Geological Society of America, 2015, pp.1-15. ⟨10.1130/B31145.1⟩
Geological Society of America Bulletin, Geological Society of America, 2015, pp.1-15. ⟨10.1130/B31145.1⟩
International audience; Lakes are major depositional systems for which the related depositional processes have long been considered relatively simple. Breaking this statement, this study presents a detailed analysis of deposits in Lake Saint-Jean, th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::68ba75647de684a09333508f7f2d364c
https://hal-insu.archives-ouvertes.fr/insu-01184724
https://hal-insu.archives-ouvertes.fr/insu-01184724
Autor:
Pierre A. Cousineau, Hugues Longuépée
Publikováno v:
The Canadian Mineralogist. 44:967-980
The term glauconite covers a series of iron-rich minerals that form in the upper layer of sediments of the sea bottom in locations where sediment input is low. Because of its potassium content and the process of its formation, it is one of few minera
Autor:
Pierre A. Cousineau, Hugues Longuépée
Publikováno v:
Canadian Journal of Earth Sciences. 42:259-272
The Cambrian Anse Maranda Formation is a glauconite-bearing clastic succession within the Quebec Reentrant. It is part of the Appalachians Humber Zone, particularly of the shale feldspathic sandstone assemblage, which represents the rift-to-drift