Results 111 to 120 of about 236 (132)
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Sedimentary Geology, 2013
Abstract The interaction of ramps, basin plains and turbidite systems on the scale of tens of km has been rarely observed in fossil examples. Deep marine Eocene–Oligocene beds are exposed in the axial zone of the Chianti Mountains, Italy, and compose a regionally continue stratigraphic succession known as the Scaglia Toscana Formation.
Alessandro Ielpi, Gianluca Cornamusini
exaly +4 more sources
Abstract The interaction of ramps, basin plains and turbidite systems on the scale of tens of km has been rarely observed in fossil examples. Deep marine Eocene–Oligocene beds are exposed in the axial zone of the Chianti Mountains, Italy, and compose a regionally continue stratigraphic succession known as the Scaglia Toscana Formation.
Alessandro Ielpi, Gianluca Cornamusini
exaly +4 more sources
Rendiconti Lincei, 2010
The frontal northern part of the continental Adriatic microplate is formed by a stack of Austroalpine nappes and by the Southalpine basement and cover units. Both basement portions are now side by side, separated by the Periadriatic (Insubric) fault system, but they became juxtaposed only during the Alpine orogeny.
Raffaele Sassi +2 more
exaly +2 more sources
The frontal northern part of the continental Adriatic microplate is formed by a stack of Austroalpine nappes and by the Southalpine basement and cover units. Both basement portions are now side by side, separated by the Periadriatic (Insubric) fault system, but they became juxtaposed only during the Alpine orogeny.
Raffaele Sassi +2 more
exaly +2 more sources
THE ALBANIAN OROGEN: CONVERGENCE ZONE BETWEEN EURASIA AND THE ADRIA MICROPLATE
2006exaly +2 more sources
A study on off-fault aftershock pattern at N-Adria microplate
Journal of Seismology, 2018The spatial features of the aftershock sequences triggered by three moderate magnitude events with coda-duration magnitudes 4.1, 5.1 and 5.6, which occurred in Northeastern Italy and Western Slovenia, were investigated. The fractal dimension and the orientations of the planar features fitting the hypocentral data have been inferred.
Gianni Bressan +3 more
openaire +1 more source
Periodico di Mineralogia, 2014
Cretaceous to Eocene sandstones from the Southeastern Alps and Outer Dinarides (Italy, Slovenia and Croatia) have been geochemically determined to detect their provenance. The first arenaceous strata of the Julian Basin are strongly chemically influenced by the disgregation of metamorphic and not-metamorphic rock types related to the ancient Vardar sea
DE MIN, ANGELO +2 more
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Cretaceous to Eocene sandstones from the Southeastern Alps and Outer Dinarides (Italy, Slovenia and Croatia) have been geochemically determined to detect their provenance. The first arenaceous strata of the Julian Basin are strongly chemically influenced by the disgregation of metamorphic and not-metamorphic rock types related to the ancient Vardar sea
DE MIN, ANGELO +2 more
openaire +2 more sources
Is the Adria a promontory or exists as an independent microplate?
1999*
Čolić, Krešimir, Pribičević, Boško
openaire +2 more sources
2019
The red colored hematite-bearing granite from Mt. Požeška Gora and albite rhyolite that shows well-exposed phenomenon of columnar jointing from Rupnica locality have similar geochemical signature pointing to highly fractionated and high-temperature A-type of magma.
Schneider, Petra +3 more
openaire +3 more sources
The red colored hematite-bearing granite from Mt. Požeška Gora and albite rhyolite that shows well-exposed phenomenon of columnar jointing from Rupnica locality have similar geochemical signature pointing to highly fractionated and high-temperature A-type of magma.
Schneider, Petra +3 more
openaire +3 more sources
Beauty and complexity of metamorphism: case studies from the frontal part of the Adria microplate
RENDICONTI LINCEI, 2010We review a selection of case studies that highlight the fascination and complexity of metamorphic processes and mechanisms, as revealed in rocks from the crystalline basement of the frontal part of the Adria microplate. The examples from the Austroalpine metamorphic rocks south of the Tauern Window, and from the crystalline basement lying more ...
CESARE, BERNARDO +4 more
openaire +2 more sources
Rendiconti Lincei, 2013
Euganean Hills are a magmatic district belonging to the Veneto Volcanic Province, whose magmatism developed during an extensional tectonic regime within the Alpine orogenesis in an intra-plate setting (the Adria microplate). Mafic and ultramafic cumulus enclaves occur within the Euganean trachytes.
BARTOLI, OMAR +3 more
openaire +3 more sources
Euganean Hills are a magmatic district belonging to the Veneto Volcanic Province, whose magmatism developed during an extensional tectonic regime within the Alpine orogenesis in an intra-plate setting (the Adria microplate). Mafic and ultramafic cumulus enclaves occur within the Euganean trachytes.
BARTOLI, OMAR +3 more
openaire +3 more sources