Sketch of the geodynamic evolution of the Italian region. Dashed
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Sketch of the geodynamic evolution of the Italian region. Dashed lines
Sketch map of northeastern Sicily showing the main
Full article: Late Oligocene–early Miocene olistostromes (sedimentary mélanges) as tectono-stratigraphic constraints to the geodynamic evolution of the exhumed Ligurian accretionary complex (Northern Apennines, NW Italy)
Geodynamic evolution of the central and western Mediterranean: Tectonics vs. igneous petrology constraints - ScienceDirect
Sketch of the study area. (a) Simplified tectonic map showing the main
Geological map of the investigated area (dashed line). 1: pre-Tortonian
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Frontiers Multiple Lines of Evidence for a Potentially Seismogenic Fault Along the Central-Apennine (Italy) Active Extensional Belt–An Unexpected Outcome of the MW6.5 Norcia 2016 Earthquake
Three‐dimensional Moho topography in Italy: New constraints from receiver functions and controlled source seismology - Di Stefano - 2011 - Geochemistry, Geophysics, Geosystems - Wiley Online Library
Large-strain Elastic and Elasto-Plastic Formulations for Host-Inclusion Systems and Their Applications in Thermobarometry and Geodynamics
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