Results 1 to 10 of about 119 (92)

Alps to Apennines zircon roller coaster along the Adria microplate margin [PDF]

open access: yesScientific Reports, 2018
We have traced the particle path of high-pressure metasedimentary rocks on Elba Island, Northern Apennines, with the help of a U-Pb-Hf detrital zircon study. One quarter of the analysed zircons are surprisingly young, 41-30 Ma, with a main age peak at ca.
Sergio Rocchi
exaly   +8 more sources

Seismic anisotropy across Adria plate, from the Apennines to the Dinarides

open access: yesFrontiers in Earth Science, 2022
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 the east beneath the Dinarides.
Silvia Pondrelli   +2 more
exaly   +3 more sources

Reconsidering paleozoic differences between the Jadar block and the Drina-Ivanjica unit [PDF]

open access: yesGeološki Anali Balkanskoga Poluostrva, 2020
The peculiar Jadar block has an intervening position separating the main Neotethyan West Vardar Zone (including ophiolites of Late Jurassic age) and a passive margin lithospheric segment of the Apulia/Adria microplate referred to as the Drina-Ivanjica ...
Spahić Darko, Gaudenyi Tivadar
doaj   +1 more source

The role of the pre-Alpine polycrystalline basement in the paleogeographic configuration of multiple Neotethyan oceanic basins

open access: yesGeologija, 2021
The study provides a deeper understanding of the early Mesozoic paleogeogeographic spatial-temporal relationship by studying the two Adria-Europe intervening basement blocks.
Darko SPAHIĆ, Tivadar GAUDENYI
doaj   +1 more source

Transverse Dinaric zone of increased compression between the Kraški rob and Hrušica Regions, NE Microadria

open access: yesGeologija, 2023
The Kvarner fault divides the Microadria (Adria microplate, the Adria stable core) into the Po and Adria segments. The Istra block, which is sandwiched between the right-lateral Kvarner Fault and the left-lateral Sistiana Fault lies at the extreme ...
Ladislav Placer, Igor Rižnar, Ana Novak
doaj   +1 more source

The role of the 'Zvornik suture' for assessing the number of Neotethyan oceans: Surface - subsurface constraints on the fossil plate margin (Vardar Zone vs. Inner Dinarides) [PDF]

open access: yesGeološki Anali Balkanskoga Poluostrva, 2020
The balancing exercise of the “single-ocean model” and reexa - mination of Jurassic paleogeographic conditions and tectonic interaction allowed the reconstruction of the mosaic of independent microplate margins and sutured northwestern Tethyan realm ...
Spahić Darko, Gaudenyi Tivadar
doaj   +1 more source

The Sistiana Fault and the Sistiana Bending Zone (SW Slovenia)

open access: yesGeologija, 2021
The Sistiana Fault is an alleged disjunctive deformation of Microadria in the sea bottom of the Gulf of Trieste. Onshore, it is visible only in the Sistiana Bay, but towards the northeast it soon pinches-out, in structural-geometric ...
Ladislav PLACER   +2 more
doaj   +1 more source

A focal mechanism catalogue of earthquakes that occurred in the southeastern Alps and surrounding areas from 1928–2019 [PDF]

open access: yesEarth System Science Data, 2021
We present a focal mechanism catalogue of earthquakes that occurred in the southeastern Alps and surrounding areas from 1928 to 2019. The area involved in the process of convergence between the Adria microplate and Eurasia is one of the most seismically ...
A. Saraò   +4 more
doaj   +1 more source

Tectonics and gravitational phenomena (Nanos, Slovenia)

open access: yesGeologija, 2021
The Istra Pushed Area is a specifically deformed territory of the northwestern part of the External Dinarides. It formed due to the movement of the Istra block as part of the Adriatic Microplate (Adria) towards the Dinarides since the middle Miocene ...
Ladislav PLACER   +2 more
doaj   +1 more source

Deriving a New Crustal Model of Northern Adria: The Northern Adria Crust (NAC) Model

open access: yesFrontiers in Earth Science, 2020
We presented a new 3D model of the geophysical properties of the crust (namely depth of the Moho and VP, VS, density, Young’s modulus, and shear modulus) of the northern tip of the Adria microplate that we called NAC (Northern Adria Crust).
Andrea Magrin, Giuliana Rossi
doaj   +1 more source

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