Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Lukas Nibourel"'
Publikováno v:
Swiss Journal of Geosciences, Vol 114, Iss 1, Pp 1-43 (2021)
Abstract The thermo-kinematic evolution of the eastern Aar Massif, Swiss Alps, was investigated using peak temperature data estimated from Raman spectroscopy of carbonaceous material and detailed field analyses. New and compiled temperature-time cons
Externí odkaz:
https://doaj.org/article/b0518d9bb9624b7eb5daa0f3da8382a7
Autor:
Lukas Nibourel, Joël Morgenthaler, Sandra Grazioli, Isabel Schumacher, Salome Schläfli, Thomas Galfetti, Stefan Heuberger
Publikováno v:
Journal of Structural Geology, 172
Geological maps are available for almost every region of the world and, therefore, represent the most commonly used source of information for earth scientists. Advances in computing power and the availability of digital elevation data have opened new
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::60df1da82bd4cef867025c32acefe924
https://hdl.handle.net/20.500.11850/614034
https://hdl.handle.net/20.500.11850/614034
Inversion and exhumation of crystalline basement units of passive margins is a critical stage of mountain-building processes. With a multi-methodological approach that combines 3D geological modelling and cross-section restoration at different time s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3738514579e6ded9679334c6f2a1f15a
https://doi.org/10.5194/egusphere-egu23-11654
https://doi.org/10.5194/egusphere-egu23-11654
Publikováno v:
Geology. 46:879-882
Publikováno v:
Mair, David; Lechmann, Alessandro; Herwegh, Marco; Nibourel, Lukas; Schlunegger, Fritz (2018). Linking Alpine deformation in the Aar Massif basement and its cover units – the case of the Jungfrau–Eiger mountains (Central Alps, Switzerland). Solid Earth, 9(5), pp. 1099-1122. Copernicus Publications 10.5194/se-9-1099-2018
Solid Earth, Vol 9, Pp 1099-1122 (2018)
Solid Earth, Vol 9, Pp 1099-1122 (2018)
The NW rim of the external Aar Massif was exhumed from ~ 10 km depth to its present position at 4 km elevation above sea level during several Alpine deformation stages. Different models have been proposed for the timing and nature of these stages. Re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a52fab4d53a39633a8274e4d4e879107
https://doi.org/10.5194/se-2018-49
https://doi.org/10.5194/se-2018-49
Publikováno v:
Journal of Geophysical Research: Earth Surface
Journal of Geophysical Research: Earth Surface, 2015, 120 (10), pp.2056-2079. ⟨10.1002/2015JF003541⟩
Journal of Geophysical Research: Earth Surface, American Geophysical Union/Wiley, 2015, 120 (10), pp.2056-2079. ⟨10.1002/2015JF003541⟩
Journal of Geophysical Research: Earth Surface, 2015, 120 (10), pp.2056-2079. ⟨10.1002/2015JF003541⟩
Journal of Geophysical Research: Earth Surface, American Geophysical Union/Wiley, 2015, 120 (10), pp.2056-2079. ⟨10.1002/2015JF003541⟩
International audience; Detrital provenance analyses in orogenic settings, in which sediments are collected at the outlet of a catchment, have become an important tool to estimate how erosion varies in space and time. Here we present how Raman Spectr
Autor:
Simon C. Cox, Lukas Nibourel
Publikováno v:
New Zealand Journal of Geology and Geophysics. 58:154-175
River bedload surveyed at 50 sites in Westland is dominated by Alpine Schist or Torlesse Greywacke from the Alpine Fault hanging wall, with subordinate Pounamu Ultramafics or footwall-derived Western Province rocks. Tumbling experiments found ultrama