Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Pierre-Marc Godbout"'
Publikováno v:
Scientific Data, Vol 10, Iss 1, Pp 1-12 (2023)
Abstract We present a series of 1-km spatial resolution rebound (isobase) surfaces based on publicly distributed predictions obtained from the glacio-isostatic adjustment models known as ICE-5G (VM2 L90), ICE-6G_C (VM5a) and ICE-7G_NA (VM7). Our obje
Externí odkaz:
https://doaj.org/article/2a904bb18fdc4c2ba376dfd5266a840a
Publikováno v:
Scientific Data, Vol 10, Iss 1, Pp 1-1 (2023)
Externí odkaz:
https://doaj.org/article/cb3208399eec410e964af6e47283f0fc
Autor:
Édouard G. H. Philippe, Guillaume St‐Onge, Jean‐Pierre Valet, Pierre‐Marc Godbout, Ramon Egli, Pierre Francus, Martin Roy
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 3, Pp n/a-n/a (2023)
Abstract The natural remanent magnetization (NRM) of high sedimentation rate sediments provides significant information about paleomagnetic secular variation of the Earth's magnetic field and can also potentially be used for stratigraphy. However, NR
Externí odkaz:
https://doaj.org/article/a85970f77dc347638cf56bf0160c1935
Publikováno v:
Boreas. 50:51-75
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5079cf7b379b52b62595fddc9e705e35
https://doi.org/10.1111/bor.12479
https://doi.org/10.1111/bor.12479
A new glacial geomorphology map covers approximately 415,000 km2 in a core region of the Laurentide Ice Sheet in Nunavut. The compilation builds on recent and legacy maps and is supplemented by visual digitization of glacigenic features using high-re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5fbe9b2eb41acaefa0ad0f496a6725cc
https://doi.org/10.4095/327853
https://doi.org/10.4095/327853
Publikováno v:
Quaternary Science Reviews. 274:107269
The climate variability of the last deglaciation is often linked to meltwater discharges from the melting of large ice sheets. One of the best examples comes from the drainage of glacial Lake Agassiz-Ojibway (LAO) and its attendant perturbation of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e204c8cd36c209ae5213ef9232109781
https://doi.org/10.1016/j.quascirev.2021.107269
https://doi.org/10.1016/j.quascirev.2021.107269
Publikováno v:
Quaternary Research. 88:265-276
Surface exposure dating was applied to erosional shorelines associated with the Angliers lake level that marks an important stage of Lake Ojibway. The distribution of 1510Be ages from five sites shows a main group (10 samples) of coherent10Be ages yi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d194a5a4c897eaf23535647791059328
https://doi.org/10.1017/qua.2017.40
https://doi.org/10.1017/qua.2017.40
Publikováno v:
Quaternary Science Reviews. 238:106327
Glacial Lake Ojibway occupied large areas in northeastern Ontario and northwestern Quebec during the last deglaciation. Paleogeographic reconstructions depict Lake Ojibway and Lake Agassiz sharing a common water plane shortly before the final drainag
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4156582a30f3d9fb861c57d31297df9
https://doi.org/10.1016/j.quascirev.2020.106327
https://doi.org/10.1016/j.quascirev.2020.106327
Publikováno v:
Quaternary Science Reviews. 223:105942
Lake Ojibway developed at the southern Laurentide Ice Sheet margin during the last deglaciation and covered vast expanses of northeastern Ontario and northwestern Quebec (Canada). The late-stage history of the lake is complex, presumably marked by a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::be7c88165bee5a5e35e579bc0976f9b3
https://doi.org/10.1016/j.quascirev.2019.105942
https://doi.org/10.1016/j.quascirev.2019.105942