Search results for "W Calabria continental margin"

showing 3 items of 3 documents

The architecture and Neogene to Recent evolution of the W Calabrian continental margin: an upper plate perspective to the Ionian subduction system (C…

2010

The western Calabria continental margin forms the transition between the Pliocene to Recent Marsili spreading center and continental Calabria, all parts of the upper plate of the Ionian subduction zone. Integrating high-resolution and crustal seismic images constrained by gravity modeling, we provide a detailed reconstruction of the architecture of the margin and develop a new scheme for its Miocene to present evolution. This time span encompasses the continent-continent collision between Africa and Eurasia, subsequent orogenic collapse and rifting apart between the two continental masses, and the Pliocene to Recent emplacement of oceanic crust in the Vavilov and Marsili basins. The crust o…

Extensional faultSubductionSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleCrustW Calabria continental marginNeogeneGeophysicsContinental marginGeochemistry and PetrologyOceanic crustThrust faultTyrrhenian BasinSynclineIonian subduction zoneSeismologyGeology
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Crustal architecture and Miocene to Recent evolution of the W Calabria continental margin (Southern Tyrrhenian Sea)

2008

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleW Calabria continental marginIonian subduction zone
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The transition between the Marsili oceanic crust and the W Calabria rifted margin: rifting and drifting in the upper plate of the Ionian subduction z…

2012

The western Calabria continental margin forms the transition between the Late Pliocene to Recent Marsili spreading center and continental Calabria. Integrating highpenetration and -resolution upper crustal seismic images with seafloor morphology, ODP well data and geological/geophysical constraints we provide a detailed reconstruction of the architecture of the distal portion of the W Calabria rifted margin and of the adjacent Marsili “oceanic” domain (Fig. 1) and develop a scheme for the Pliocene to present rifting and drifting of the upper plate of the Ionian subduction zone. Our seismic data document the presence of stretched and thinned continental crust, less than 10 Km thick into the …

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaW Calabria continental margin Continent– Ocean Transition; Mantle exhumation; Marsili basin Marsili volcano Southern Tyrrhenian Sea.Mantle exhumationMarsili basin Marsili volcano Southern Tyrrhenian Sea.W Calabria continental margin Continent– Ocean Transition
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