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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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Gastrointestinal absorption, tissue retention, and urinary excretion of dietary aluminum in rats determined by using 26Al

TL;DR: Using accelerator mass spectrometry and 26AI to study the plasma concentration, urinary excretion, and retention in bone, brain, and liver of a single dose of a dietary concentration of aluminum ingested either with or without citrate by 2-month-old Wistar rats found this factor was highly variable in individual rats.
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Measurement of 10Be with a tandetron accelerator operating at 2 MV

TL;DR: In this article, a General Ionex Corporation Tandetron accelerator mass spectrometer system, operating at a nominal terminal voltage of 2 MV, has been used to measure 10Be.
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Rapid Holocene Deglaciation of the Labrador Sector of the Laurentide Ice Sheet

TL;DR: In this article, new 10Be cosmogenic exposure ages on glacially deposited boulders are used to date the final disappearance of the Labrador sector of the Laurentide Ice Sheet (LS-LIS).
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The AMS facility at Gif-sur-Yvette: progress, perturbations and projects

TL;DR: In this paper, the authors report on developments at the Gif-sur-Yvette AMS facility since 1990, including the installation of a new dual port injection line based on a rotating electrostatic analyzer designed and constructed by IsoTrace laboratory.
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Glacial survival of blockfields on the Varanger Peninsula, northern Norway

TL;DR: In this paper, the relationship between blockfields, developed in quartzites and sandstones on the Varanger Peninsula, northern Norway, and glacially derived features have been evaluated and it was concluded that the blockfields have survived underneath at least one thick, cold-based ice sheet.