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Maarten Lupker

Researcher at ETH Zurich

Publications -  59
Citations -  2094

Maarten Lupker is an academic researcher from ETH Zurich. The author has contributed to research in topics: Sediment & Cosmogenic nuclide. The author has an hindex of 17, co-authored 53 publications receiving 1559 citations. Previous affiliations of Maarten Lupker include University of Lorraine & Centre national de la recherche scientifique.

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Mineralogical and chemical variability of fluvial sediments 2. Suspended-load silt (Ganga–Brahmaputra, Bangladesh)

TL;DR: In this article, the authors combined Raman spectroscopy with traditional heavy-mineral and X-ray diffraction analyses, carried out separately on low-density and dense fractions of all significant size classes in each sample.
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Predominant floodplain over mountain weathering of Himalayan sediments (Ganga basin)

TL;DR: In this paper, the authors present an extensive river sediment dataset covering the Ganga basin from the Himalayan front downstream to the ganga mainstream in Bangladesh and show that the Gangetic floodplain is the dominant location of silicate weathering for Na, K and [H2O + ].
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Increasing chemical weathering in the Himalayan system since the Last Glacial Maximum

TL;DR: In this article, a composite sediment record from the Bay of Bengal is used to document the evolution of chemical weathering in the Himalayan system (Himalayan range and Indo-Gangetic floodplain), the world largest sediment conveyor to the oceans, since the Last Glacial Maximum (LGM).
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A Rouse-based method to integrate the chemical composition of river sediments: Application to the Ganga basin

TL;DR: Lupker et al. as discussed by the authors used a Rouse-based method to integrate the chemical composition of river sediments to derive the annual flux and grain size distributions of the sediments.
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10Be-derived Himalayan denudation rates and sediment budgets in the Ganga basin

TL;DR: In this paper, in situ-produced cosmogenic 10 Be concentrations were measured in detritic quartz in order to determine basin-scale denudation rates for the central part of the Himalayan range.