'Conjugate'coseismic surface faulting related with the 29 December 2020, Mw 6.4, Petrinja earthquake (Sisak-Moslavina, Croatia)
We provide here a first-hand description of the coseismic surface effects caused by the Mw
6.4 Petrinja earthquake that hit central Croatia on 29 December 2020. This was one of the …
6.4 Petrinja earthquake that hit central Croatia on 29 December 2020. This was one of the …
[HTML][HTML] Orogenic lithosphere and slabs in the greater Alpine area–interpretations based on teleseismic P-wave tomography
MR Handy, SM Schmid, M Paffrath, W Friederich… - Solid Earth, 2021 - se.copernicus.org
Based on recent results of AlpArray, we propose a new model of Alpine collision that
involves subduction and detachment of thick (∼ 180 km) European lithosphere. Our …
involves subduction and detachment of thick (∼ 180 km) European lithosphere. Our …
Crustal Thinning From Orogen to Back‐Arc Basin: The Structure of the Pannonian Basin Region Revealed by P‐to‐S Converted Seismic Waves
We present the results of P‐to‐S receiver function analysis to improve the 3D image of the
sedimentary layer, the upper crust, and lower crust in the Pannonian Basin area. The …
sedimentary layer, the upper crust, and lower crust in the Pannonian Basin area. The …
Post-collisional mantle delamination in the Dinarides implied from staircases of Oligo-Miocene uplifted marine terraces
The Dinarides fold-thrust belt on the Balkan Peninsula resulted from convergence between
the Adriatic and Eurasian plates since Mid-Jurassic times. Under the Dinarides, S-wave …
the Adriatic and Eurasian plates since Mid-Jurassic times. Under the Dinarides, S-wave …
Geological effects and tectonic environment of the 26 November 2019, Mw 6.4 Durres earthquake (Albania)
E Vittori, AM Blumetti, V Comerci… - Geophysical Journal …, 2021 - academic.oup.com
SUMMARY The M w 6.4 26 November 2019, earthquake has been the strongest in the last
decades in Albania, causing damages of intensity VIII to IX EMS in the epicentral region …
decades in Albania, causing damages of intensity VIII to IX EMS in the epicentral region …
Seismic attenuation tomography of Eastern Europe from ambient seismic noise analysis
SUMMARY The Eastern-Europe region (EER), is a complex geotectonic area that captures
part of the Alpine-Himalayan Orogen, the subduction of multiple NeoTethys Branches and …
part of the Alpine-Himalayan Orogen, the subduction of multiple NeoTethys Branches and …
Constraints on Complex Faulting during the 1996 Ston–Slano (Croatia) earthquake inferred from the DInSAR, seismological, and geological observations
This study, involving remote sensing, seismology, and geology, revealed complex faulting
during the mainshock of the Ston–Slano earthquake sequence (5 September, 1996, Mw …
during the mainshock of the Ston–Slano earthquake sequence (5 September, 1996, Mw …
High-resolution crustal S-wave velocity model and Moho geometry beneath the Southeastern Alps: New insights from the SWATH-D experiment
We compiled a dataset of continuous recordings from the temporary and permanent seismic
networks to compute the high-resolution 3D S-wave velocity model of the Southeastern Alps …
networks to compute the high-resolution 3D S-wave velocity model of the Southeastern Alps …
Geophysical‐petrological model for bidirectional mantle delamination of the Adria microplate beneath the northern Apennines and Dinarides orogenic systems
This study presents a geophysical‐geochemical integrated model of the thermochemical
structure of the lithosphere and uppermost mantle along a transect from the Northern …
structure of the lithosphere and uppermost mantle along a transect from the Northern …
Seismic anisotropy across Adria plate, from the Apennines to the Dinarides
The Adria microplate has the particular feature to be involved in two subduction systems with
slab dipping in opposite directions, one toward west beneath the Apennines and the other to …
slab dipping in opposite directions, one toward west beneath the Apennines and the other to …