Results 51 to 60 of about 119 (92)
Abstract The eastern Adriatic margin is composed by an Ocean‐Continent Transition lithosphere (OCT), resulting in the southwards along‐strike variation from collision to subduction. The Cephalonia‐Lefkada Transform Fault zone (CTF) is a right‐lateral strike‐slip fault system located above the OCT and associated to this kinematic transition.
Silvia Crosetto +6 more
wiley +1 more source
Adria microplate: a puzzling key stone in west-central Mediterranean geodynamics
ISSN:1593 ...
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Supplemental Material: The two-sided continental subduction of the Adria microplate (Mediterranean)
<p>Additional figures (S1–S5) and a text analyzing Vp and Vp/Vs perturbations at lithospheric mantle depths, synthetic slab test beneath the Dinarides, checkerboard and recovery tests for the Adria plate, comparisons with previous tomographic studies, and a detailed discussion of the observed velocity anomalies and model comparisons. </p>
et al., Irene Menichelli
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<p>The Late Cretaceous magmatic rocks within the southwestern part of the Pannonian Basin basement (Croatia) occur in two areas: Vo&#263;in volcanic mass (VVM) at the northwestern part of Mt. Papuk (near town of Vo&#263;in, covering the area of ~10km<sup>2</sup>) and volcanic mass of Mt.
Petra Schneider, Dražen Balen
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Present-Day Structure of the Adria Microplate and its Evolution Through Time
The current upper crustal and in-depth tectonic structures and evolution of the Adria microplate, located between the large Eurasian and African tectonic plates, have been the primary focus of numerous scientific publications. These studies have concluded a wide range of interpretations, some of which are contradictory, since the earliest paleotectonic
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Supported by evidence of deep crustal sources for the observed magnetic anomalies in Central Italy and by outcropping gabbros in the Croatian archipelago, we model the observed gravity and magnetic anomalies in the Central Adriatic Sea and surroundings.
Fabio Speranza +2 more
exaly +2 more sources
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SEISMICITY ALONG THE NORTHWESTERN EDGE OF THE ADRIA MICROPLATE
2006This contribution is an overview of the seismic activity observed along the northwestern edge of the Adria microplate over the last 15 years. The study area stretches from Lyons to Turin, and from Geneva to Nice. The discussion focuses on several key zones where significant earthquakes occurred during this period, or where the connection between ...
François Thouvenot
exaly +4 more sources
AbstractThis study presents a geophysical‐geochemical integrated model of the thermochemical structure of the lithosphere and uppermost mantle along a transect from the Northern Tyrrhenian Sea to the Pannonian Basin, crossing the northern Apennines, the Adriatic Sea, and the Dinarides fold‐thrust belt.
Montserrat Torné i Escasany +2 more
exaly +5 more sources
Tertiary geodynamic evolution of the Southern Adria microplate
Terra Nova, 1996ABSTRACTThe southern Adria microplate is the common foreland for the Hellenide and Southern Apennine thrust belts. The Apulian Platform dominates the microplate; outcrop, well and seismic data allow us to trace the carbonate platform edge, whilst structural analysis, geophysical and palaeomagnetic data provide important clues to the geodynamic ...
Roberto Gambini, Mario Tozzi
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Subduction Zones Interaction Around the Adria Microplate and the Origin of the Apenninic Arc
Tectonics, 2018AbstractThe study of slab‐slab interactions has come to the front of geodynamics researches to explain geological and geophysical observations from tectonically complex areas. Here we aim to better understand the geodynamics of the Central Mediterranean, where the Adria plate subducts on its two opposite sides.
Francesca Funiciello +2 more
exaly +3 more sources

