Zobrazeno 1 - 10
of 93
pro vyhledávání: '"Françoise Yiou"'
Autor:
Lyn Gualtieri, Françoise Yiou, Grant M. Raisbeck, Edward J. Brook, Jon Y. Landvik, Henriette Linge, Otto Salvigsen
Publikováno v:
Boreas. 42:43-56
The Late Weichselian ice sheet of western Svalbard was characterized by ice streams and inter-ice-stream areas. To reconstruct its geometry and dynamics we investigated the glacial geology of two areas on the island of Prins Karls Forland and the Mit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::76e21e91ab9d34c64bbcc617d6beeebb
https://doi.org/10.1111/j.1502-3885.2012.00282.x
https://doi.org/10.1111/j.1502-3885.2012.00282.x
Autor:
Grant M. Raisbeck, Vincent Rinterknecht, Peter U. Clark, Françoise Yiou, Leszek Marks, Jan A. Piotrowski, Edward J. Brook
Publikováno v:
Boreas. 34:186-191
Rinterknecht, V. R., Marks, L., Piotrowski, J. A., Raisbeck, G. M., Yiou, F., Brook, E. J. & Clark, P. U. 2005 (May): Cosmogenic 10Be ages on the Pomeranian Moraine, Poland. Boreas, Vol. 34, pp. 186–191. Oslo. ISSN 0300–9483. We measured the 10Be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c85a831ed469d96f0895f94413f2276d
https://doi.org/10.1111/j.1502-3885.2005.tb01014.x
https://doi.org/10.1111/j.1502-3885.2005.tb01014.x
Publikováno v:
Quaternary Science Reviews
Quaternary Science Reviews, Elsevier, 2008, 27, pp.320-336. ⟨10.1016/j.quascirev.2007.11.004⟩
Quaternary Science Reviews, Elsevier, 2008, 27, pp.320-336. ⟨10.1016/j.quascirev.2007.11.004⟩
The margins of the Fennoscandian Ice Sheet (FIS) during the Last Glacial Maximum (LGM) are fairly well constrained, yet the thickness of the FIS and its temporal evolution are poorly known. Here, we use beryllium-10 (Be-10) exposure ages of glacially
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::83f4666bf35bcf7e872bf46f331fc872
https://doi.org/10.1016/j.quascirev.2007.11.004
https://doi.org/10.1016/j.quascirev.2007.11.004
Publikováno v:
Quaternary Science Reviews
Quaternary Science Reviews, 2007, 26 (17-18), pp.2301-2304. ⟨10.1016/j.quascirev.2007.06.002⟩
Quaternary Science Reviews, Elsevier, 2007, 26 (17-18), pp.2301-2304. ⟨10.1016/j.quascirev.2007.06.002⟩
Quaternary Science Reviews, 2007, 26 (17-18), pp.2301-2304. ⟨10.1016/j.quascirev.2007.06.002⟩
Quaternary Science Reviews, Elsevier, 2007, 26 (17-18), pp.2301-2304. ⟨10.1016/j.quascirev.2007.06.002⟩
International audience
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a6c8e46005a5b8f229bd9db786aeb1eb
https://doi.org/10.1016/j.quascirev.2007.06.002
https://doi.org/10.1016/j.quascirev.2007.06.002
Autor:
Grant M. Raisbeck, Irina E. Pavlovskaya, Vincent Rinterknecht, Françoise Yiou, Peter U. Clark, Edward J. Brook
Publikováno v:
Boreas. 36:307-313
We measured 10Be concentrations in boulders collected from the Orsha and Braslav moraines, associated with the Last Glacial Maximum extent and a recessional stage of the Scandinavian Ice Sheet (SIS), respectively, providing a direct dating of the sou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a5a531007ef11b6ab55a4c4352f2f07e
https://doi.org/10.1111/j.1502-3885.2007.tb01252.x
https://doi.org/10.1111/j.1502-3885.2007.tb01252.x
Autor:
Grant M. Raisbeck, Svein Olaf Dahl, Danny McCarroll, Edward J. Brook, Atle Nesje, Colin K. Ballantyne, Henriette Linge, Françoise Yiou
Publikováno v:
Boreas. 36:227-239
Blockfields, weathering boundaries and marginal moraines have been mapped along a longitudinal transect from northern Andoya to Skanland in northern Norway. The degree of rock-surface weathering above and below glacial trimlines, clay-mineral assembl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c088dffdad55f6b63dd0aef47eb9bb4
https://doi.org/10.1111/j.1502-3885.2007.tb01247.x
https://doi.org/10.1111/j.1502-3885.2007.tb01247.x
Autor:
Grant M. Raisbeck, Leif Sørbel, Françoise Yiou, Henriette Linge, Edward J. Brook, Jakob Fjellanger
Publikováno v:
Geomorphology
Geomorphology, Elsevier, 2006, 82, pp.255-272. ⟨10.1016/j.geomorph.2006.05.007⟩
Geomorphology, Elsevier, 2006, 82, pp.255-272. ⟨10.1016/j.geomorph.2006.05.007⟩
For more than hundred years it has been debated whether blockfields in mountain summit areas can be used to delimit the vertical extent of Pleistocene ice sheets. In this study the relationship between blockfields, developed in quartzites and sandsto
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fe56a82707ed0980563bc87056bef05c
https://doi.org/10.1016/j.geomorph.2006.05.007
https://doi.org/10.1016/j.geomorph.2006.05.007
Autor:
Eleanor Bennett, Richard J. Norris, Françoise Yiou, J. H. Youngson, James Jackson, Grant M. Raisbeck
Publikováno v:
New Zealand Journal of Geology and Geophysics. 49:217-231
Measurements of 10Be concentrations in quartz‐rich boulders exposed by the uplift of anticlinal ranges in Central Otago, New Zealand, are used to investigate the fault propagation styles and rates for the underlying blind reverse faults. 10Be ages
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e14de2376ec4cfdaf4161514bebe5e3d
https://doi.org/10.1080/00288306.2006.9515161
https://doi.org/10.1080/00288306.2006.9515161
Autor:
Françoise Yiou, Silvio Tschudi, Peter U. Clark, Grant M. Raisbeck, Vincent Rinterknecht, Juha P. Lunkka, Edward J. Brook
Publikováno v:
Quaternary Science Reviews
Quaternary Science Reviews, Elsevier, 2004, 23 (23-24), pp.2283-2289. ⟨10.1016/j.quascirev.2004.06.012⟩
Quaternary Science Reviews, Elsevier, 2004, 23 (23-24), pp.2283-2289. ⟨10.1016/j.quascirev.2004.06.012⟩
We determined in situ cosmogenic 10Be ages for nine boulders sampled on the Salpausselka I (Ss I) Moraine. Previous dating of this moraine indicated that it formed during the Younger Dryas Stadial along the southern margin of the Scandinavian Ice She
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e84a0f7faddd8d69744942ac62807572
https://doi.org/10.1016/j.quascirev.2004.06.012
https://doi.org/10.1016/j.quascirev.2004.06.012
Publikováno v:
Earth and Planetary Science Letters. 227:281-296
The transition from 41- to 100-kyr glacial cycles and concomitant increase in global ice volume ~1 Ma remain an enigmatic feature of late Cenozoic climate. Here, we examine the petrology, mineralogy, and geochemistry of the silicate fraction of tills
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2139dfc1906b66528da91f1abf2ed6a6
https://doi.org/10.1016/j.epsl.2004.09.001
https://doi.org/10.1016/j.epsl.2004.09.001