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Didier Bourlès

Researcher at Aix-Marseille University

Publications -  309
Citations -  12960

Didier Bourlès is an academic researcher from Aix-Marseille University. The author has contributed to research in topics: Glacial period & Cosmogenic nuclide. The author has an hindex of 61, co-authored 301 publications receiving 11171 citations. Previous affiliations of Didier Bourlès include Aster & Université Paul Cézanne Aix-Marseille III.

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Production of cosmogenic radionuclides at great depth: A multi element approach

TL;DR: In this paper, an approach to investigate in situ produced cosmogenic nuclides 10 Be, 26 Al and 36 Cl along a single 11-meter long core drilled from the surface and composed of carbonates and quartzose conglomerates has been launched.
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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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The French accelerator mass spectrometry facility ASTER: Improved performance and developments

TL;DR: Following the installation and acceptance test of the French 5 MV AMS facility ASTER, the focus has been on improving the capability for routine measurements of 10Be and 26Al as discussed by the authors.
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Slope instability in relation to glacial debuttressing in alpine areas (Upper Durance catchment, southeastern France): Evidence from field data and 10Be cosmic ray exposure ages

TL;DR: In this article, the role of deglacial unloading and resulting paraglacial stress release in conditioning or triggering slope failure is investigated, and it is shown that major rock falls and rock avalanches are associated with areas subject to the highest decompression stresses.
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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.