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Peter W. Kubik

Researcher at ETH Zurich

Publications -  262
Citations -  17890

Peter W. Kubik is an academic researcher from ETH Zurich. The author has contributed to research in topics: Glacial period & Glacier. The author has an hindex of 68, co-authored 262 publications receiving 16373 citations. Previous affiliations of Peter W. Kubik include Paul Scherrer Institute & École Polytechnique Fédérale de Lausanne.

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Surface exposure dating of Late Pleistocene glaciations at the Dedegöl Mountains (Lake Beyşehir, SW Turkey)

TL;DR: In this paper, the Muslu valley in the western central Taurus Mountains of SW Anatolia has been studied and the authors show evidence for pronounced glacier advances prior to the global Last Glacial Maximum (LGM; 21 ± 2 ka).
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Glacier response to the change in atmospheric circulation in the eastern Mediterranean during the Last Glacial Maximum

TL;DR: In this article, the authors document glacial deposits and reconstruct the glacial history in the Karagol valley system in the eastern Uludag in northwestern Turkey based on 42 cosmogenic 10Be exposure ages from boulders and bedrock.
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Debris-flow–dependent variation of cosmogenically derived catchment-wide denudation rates

TL;DR: In this article, the authors used a time series (3 yr) in the Aare catchment (central Swiss Alps) to test the impact of spatially heterogeneous stochastic sediment supply on CWDRs.
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An improved experimental determination of cosmogenic 10Be/21Ne and 26Al/21Ne production ratios in quartz

TL;DR: Goethals et al. as mentioned in this paper used surface samples from the 760-±-2-ka old Bishop Tuff in eastern California to quantify the 10 Be/21 Ne and 26 Al/ 21 Ne production rate ratios in quartz.
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Surface exposure dating of moraines in the Kromer valley (Silvretta Mountains, Austria)-evidence for glacial response to the 8.2 ka event in the Eastern Alps?:

TL;DR: In this paper, a pronounced glacier advance (Kromer stadial) in the western part of the Silvretta Mountains (western Austria) yielded ages ranging from 8010±360 to 8690±410 years.