Regional beryllium-10 production rate for the mid-elevation mountainous regions in central Europe, deduced from a multi-method study of moraines and lake sediments in the Black Forest

Autor: F. M. Hofmann, C. Rambeau, L. Gegg, M. Schulz, M. Steiner, A. Fülling, L. Léanni, F. Preusser

Publikováno v: Geochronology, Vol 6, Pp 147-174 (2024)

Beryllium-10 cosmic-ray exposure (CRE) dating has revolutionized our understanding of glacier fluctuations around the globe. A key prerequisite for the successful application of this dating method is the determination of regional production rates of

Externí odkaz: https://doaj.org/article/cdb407d2d5e648959be16026111e0fd2

Late glacial deglaciation of the Zackenberg area, NE Greenland

Autor: J. Garcia-Oteyza, M. Oliva, D. Palacios, J.M. Fernández-Fernández, I. Schimmelpfennig, N. Andrés, D. Antoniades, H.H. Christiansen, O. Humlum, L. Léanni, V. Jomelli, J. Ruiz-Fernández, V. Rinterknecht, T.P. Lane, K. Adamson, Georges Aumaître, Didier Bourlès, Karim Keddadouche

Publikováno v: Scopus
Geomorphology
Geomorphology, 2022, 401, pp.108125. ⟨10.1016/j.geomorph.2022.108125⟩
RUO. Repositorio Institucional de la Universidad de Oviedo
instname

The Greenland Ice Sheet (GrIS) is a key component of the global climate system. However, our current understanding of the spatio-temporal oscillations and landscape transformation of the GrIS margins since the last glacial cycle is still incomplete.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c21d3b3c48f462f3f78d3b9e17d3e0d6
http://hdl.handle.net/10651/64960

A karstic model of the generation of tablelands landscapes in sandstones in Eastern Amazonia

Autor: H.N. Barreto, R. Braucher, A.A.R. Salgado, L. Siame, L. Léanni, A. Auler, F.P. Martins, D.L. Bourlès

Publikováno v: Journal of South American Earth Sciences. 114:103709

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::83a0cb0bd6a4fb517b309dd0e50dded0
https://doi.org/10.1016/j.jsames.2021.103709

Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.

Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.