ForschungAG Hampel
Publikationen

Publikationen der AG Hampel

Tektonik, Strukturgeologie und tektonische Geomorphologie


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2020


Brune S, Baes M, Gerya TV, Sobolev SV. Interaction of a mantle plume and a moving plate: insights from numerical modeling

. in EGU 2020. doi.org/10.5194/egusphere-egu2020-8187. 2020


2019


Baes M, Sobolev SV, Gerya TV, Brune S. Addressing subduction initiation: A key – but unresolved – feature of plate tectonics. in Geophysical Research Abstracts Vol. 21: EGU2019-5956. Wien: General Assembly European Geosciences Union. 2019

Bagge M, Hampel A, Gold R. Modeling the Holocene slip history of the Wasatch fault (Utah): Coseismic and postseismic Coulomb stress changes and implications for paleoseismicity and seismic hazard. Bulletin of the Geological Society of America. 2019 Jan 1;131(1-2):43-57.

doi.org/10.1130/b31906.1

Hampel A, Lüke J, Krause T, Hetzel R. Finite-element modelling of glacial isostatic adjustment (GIA): use of elastic foundations at material boundaries versus the geometrically non-linear formulation. Computers and Geosciences. 2019 Jan;122(122):1-14.

doi.org/10.1016/j.cageo.2018.08.002

Heineke C, Hetzel R, Nilius NP, Zwingmann H, Todd A, Mulch A et al. Detachment faulting in a bivergent core complex constrained by fault gouge dating and low-temperature thermochronology. Journal of structural geology. 2019 Okt;127. 103865.

doi.org/10.1016/j.jsg.2019.103865

Heineke C, Hetzel R, Nilius N-P, Glotzbach C, Akal C, Christl M et al. Spatial patterns of erosion and landscape evolution in a bivergent metamorphic core complex revealed by cosmogenic 10Be: The central menderes massif (western Turkey). Geosphere. 2019 Dez 1;15(6):1846-1868.

doi.org/10.1130/GES02013.1

,

doi.org/10.15488/9313

Hetzel R, Hampel A, Gebeken P, Xu Q, Gold R. A constant slip rate for the western Qilian Shan frontal thrust during the last 200 ka consistent with GPS-derived and geological shortening rates. Earth and Planetary Science Letters. 2019 Mär 1;509(509):100-113.

doi.org/10.1016/j.epsl.2018.12.032


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