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Grant M. Raisbeck

Researcher at Centre national de la recherche scientifique

Publications -  129
Citations -  13116

Grant M. Raisbeck is an academic researcher from Centre national de la recherche scientifique. The author has contributed to research in topics: Ice core & Ice sheet. The author has an hindex of 54, co-authored 129 publications receiving 12285 citations. Previous affiliations of Grant M. Raisbeck include Oregon State University & Université Paris-Saclay.

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Chronology of Taylor Glacier Advances in Arena Valley, Antarctica, Using in Situ Cosmogenic 3He and 10Be

TL;DR: In situ produced cosmogenic nuclides provide a new technique for constraining exposure ages of glacial deposits as mentioned in this paper, and the exposure ages appear consistent with the few previous age estimates, particularly with an isotope stage 5 age for Taylor II.
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129I from nuclear fuel reprocessing facilities at Sellafield (U.K.) and La Hague (France); potential as an oceanographie tracer

TL;DR: In this paper, the authors estimate that the amount of 129I (half-life 16 m.y.) transferred to the oceans from the nuclear fuel reprocessing facilities at La Hague, France and Sellafield, Great Britain during the past 25 years has been ~ 5 X 1027 atoms, or ~ 1.2 ton of the isotope.
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Estimation of slip rates in the southern Tien Shan using cosmic ray exposure dates of abandoned alluvial fans

TL;DR: In this article, the relationship between cosmogenic nuclide content of individual clasts and the time since their deposition on a surface was assessed, and it was shown that very low 10 Be concentrations in material from active streambeds and at depth below one of the fan surfaces indicate that exposure prior to deposition onto fan surfaces was minimal.
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10 Be evidence for the Matuyama–Brunhes geomagnetic reversal in the EPICA Dome C ice core

TL;DR: Evidence is presented for enhanced 10Be deposition in the ice at 3,160–3,170 m, which is interpreted as a result of the low dipole field strength during the Matuyama–Brunhes geomagnetic reversal, which occurred about 780,000 years ago and provides a crucial tie point between ice cores, marine cores and a radiometric timescale.