Lithospheric memory, state of stress and rheology: neotectonic controls on Europe's intraplate continental topography
S Cloetingh, PA Ziegler, F Beekman… - Quaternary Science …, 2005 - Elsevier
To date, research on neotectonics and related continental topography development has
mostly focused on active plate boundaries characterized by generally high deformation …
mostly focused on active plate boundaries characterized by generally high deformation …
Lithosphere tectonics and thermo-mechanical properties: an integrated modelling approach for Enhanced Geothermal Systems exploration in Europe
Knowledge of temperature at drillable depth is a prerequisite in site selection for geothermal
exploration and development of enhanced geothermal systems (EGS). Equally important …
exploration and development of enhanced geothermal systems (EGS). Equally important …
Evolution of the European Cenozoic Rift System: interaction of the Alpine and Pyrenean orogens with their foreland lithosphere
The evolution of the European Cenozoic Rift System (ECRIS) and the Alpine orogen is
discussed on the base of a set of palaeotectonic maps and two retro-deformed lithospheric …
discussed on the base of a set of palaeotectonic maps and two retro-deformed lithospheric …
Crustal evolution of western and central Europe
PA Ziegler, P Dèzes - Geological Society, London, Memoirs, 2006 - lyellcollection.org
A new Moho depth map has been assembled for Western and Central Europe and the
Western Mediterranean area that is exclusively based on published regional Moho depth …
Western Mediterranean area that is exclusively based on published regional Moho depth …
Post-Variscan evolution of the lithosphere in the Rhine Graben area: constraints from subsidence modelling
PA Ziegler, ME Schumacher, P Dèzes… - Geological Society …, 2004 - lyellcollection.org
In the area of the Cenozoic Rhine rift system, crustal and lithospheric thicknesses range
between 24 and 35 km, and 60 and 120 km, respectively. This rift system transects the …
between 24 and 35 km, and 60 and 120 km, respectively. This rift system transects the …
Element partitioning between immiscible carbonatite–kamafugite melts with application to the Italian ultrapotassic suite
Trace element partition coefficients between conjugate carbonatite–silicate melts are a
suitable tool to test whether such natural magmas originated by liquid immiscibility. In the …
suitable tool to test whether such natural magmas originated by liquid immiscibility. In the …
Present-day 3D structural model of the Po Valley basin, Northern Italy
C Turrini, O Lacombe, F Roure - Marine and Petroleum Geology, 2014 - Elsevier
A 3D structural model of the Po Valley basin (Northern Italy) was built by integrating the
dataset available from the public domain (DEM, wells, isobath-maps, cross-sections, outcrop …
dataset available from the public domain (DEM, wells, isobath-maps, cross-sections, outcrop …
Evolution of the lithosphere in the area of the Rhine Rift System
PA Ziegler, P Dèzes - International Journal of Earth Sciences, 2005 - Springer
Abstract The Rhine Rift System (RRS) forms part of the European Cenozoic Rift System
(ECRIS) and transects the Variscan Orogen, Permo-Carboniferous troughs and Late …
(ECRIS) and transects the Variscan Orogen, Permo-Carboniferous troughs and Late …
Late Miocene shortening of the Northern Apennines back-arc
Abstract The inner Northern Apennines (western Tuscany and Tyrrhenian basin) is
characterized by a relatively thin continental crust (∼ 20–25 km), high heat flow (> 100 mW …
characterized by a relatively thin continental crust (∼ 20–25 km), high heat flow (> 100 mW …
Neotectonics and intraplate continental topography of the northern Alpine Foreland
S Cloetingh, T Cornu, PA Ziegler, F Beekman… - Earth-Science …, 2006 - Elsevier
Research on neotectonics and related seismicity has hitherto been mostly focused on active
plate boundaries that are characterized by generally high levels of earthquake activity …
plate boundaries that are characterized by generally high levels of earthquake activity …