Alle Publikationen am Institut
Zeige Ergebnisse 211 - 220 von 322
2014
Baes M, Sobolev SV. subduction initiation: Insights from numerical models. in German Swiss Geodynamics Workshop. Bad Münster am Stein, Germany. 2014
Baes M, Sobolev SV. Subduction initiation triggered by mantle suction flow. in EGU 2014. 2014
Brandes C, Tanner DC. Fault-related folding: A review of kinematic models and their application. Earth-Science Reviews. 2014 Nov 1;138:352-370. doi: 10.1016/j.earscirev.2014.06.008
Dinis J, Mendes M, Dinis P, Pais J, Rey J, Heimhofer U. Clays and Vegetation: Comparing Palaeoclimatic Signatures in the Portuguese Lower Cretaceous. in Springer Geology. Springer. 2014. S. 649-653. (Springer Geology). doi: 10.1007/978-3-319-04364-7_124
Gerya TV, Stern RJ, Baes M, Sobolev SV, Whattam S. Dynamics and Significance of Plume-Induced Subduction Initiation: Numerical Modeling. in AGU 2014. 2014
Glotzbach C, Brandes C. Air density of the Permian atmosphere: Constraints from lithified raindrop imprints. Palaeogeography, Palaeoclimatology, Palaeoecology. 2014 Sep 1;409:280-289. doi: 10.1016/j.palaeo.2014.05.024
Glotzbach C, Röttjer M, Hampel A, Hetzel R, Kubik PW. Quantifying the impact of former glaciation on catchment-wide denudation rates derived from cosmogenic 10Be. TERRA NOVA. 2014 Jun;26(3):186-194. doi: 10.1111/ter.12085
Horikx M, Heimhofer U, Dinis J, Huck S. Integrated stratigraphy of shallow marine Albian strata from the southern Lusitanian Basin of Portugal. Newsletters on stratigraphy. 2014 Jan;47(1):85-106. doi: 10.1127/0078-0421/2014/0041
Huck S, Stein M, Immenhauser A, Skelton PW, Christ N, Föllmi KB et al. Response of proto-North Atlantic carbonate-platform ecosystems to OAE1a-related stressors. Sedimentary geology. 2014 Nov 1;313:15-31. doi: 10.1016/j.sedgeo.2014.08.003
Krencker FNF, Bodin S, Hoffmann R, Suan G, Mattioli E, Kabiri L et al. The Middle Toarcian Cold Snap: Trigger of Mass Extinction and Carbonate Factory Demise. Global and Planetary Change. 2014;117:64–78. doi: 10.1016/j.gloplacha.2014.03.008
