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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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Evidence for two intervals of enhanced 10 Be deposition in Antarctic ice during the last glacial period

TL;DR: In this article, the authors measured a much more detailed concentration profile for 10Be in the Vostok core, and showed that the peak occurred at ∼60,000 yr BP.
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Quaternary Climate Change and the Formation of River Terraces across Growing Anticlines on the North Flank of the Tien Shan, China

TL;DR: In this paper, the authors infer that this spacing is due to alternating stages of valley widening and rapid incision associated with climate changes with a periodicity of 100 kyr and infer that flood plains, which were abandoned to form the terraces, developed adjacent to active stream beds during the last glacial period, when climates were relatively mild.
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Changes in the carbon cycle during the last deglaciation as indicated by the comparison of 10Be and 14C records

TL;DR: In this article, the changes in atmospheric radiocarbon (C-14) concentration during the last 50, 000 years can be attributed to changes in the C-14 production rate due to solar activity, the geomagnetic field and/or interstellar galactic cosmic ray flux.
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Slip rates of the Karakorum fault, Ladakh, India, determined using cosmic ray exposure dating of debris flows and moraines

TL;DR: In this article, Liu et al. inferred that alpine glaciers in this region have not necessarily expanded in concert with Northern Hemisphere continental ice sheets, and showed that slip along the boundaries of Tibet is not significantly more rapid than extension within the plateau.
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10Be and 9Be in marine sediments and their potential for dating

TL;DR: In this article, the fraction of the cosmogenic isotope 10Be (half-life 1.5 My), and its stable isotope 9Be, co-extracted with the following phases in marine sediments: exchangeable, calcium carbonate, Fe and Mn oxyhydroxides, organic, opal and detrital.