Search results for "MESSi"

showing 10 items of 213 documents

Paleoenvironmental changes heralding the Messinian Salinity Crisis in central Sicili: The Tripoli formation of the Falconara-Gibliscemi composite sec…

2004

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaForaminifera Stable isotopeMessinian Salinity CrisiSettore GEO/01 - Paleontologia E PaleoecologiaSettore GEO/08 - Geochimica E Vulcanologia
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Revised timing and evolution of the Messinian Salinity Crisis in the Mediterranean area

2004

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaMessinian Salinity CrisiForaminiferaSettore GEO/01 - Paleontologia E Paleoecologia
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New insights on the onset of the Messinian salinity crisis in Cyprus (East Mediterranean)

2006

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaMessinian Salinity CrisiSettore GEO/01 - Paleontologia E Paleoecologia
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Paleoenvironmental changes during the calcare di base deposition a prelude to the Messinian salinity crisis.

2006

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaMessinian Salinity Crisis Stable isotopes ForaminiferaSettore GEO/01 - Paleontologia E PaleoecologiaSettore GEO/08 - Geochimica E Vulcanologia
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Seismostratigraphic reconstruction of the Messinian palaeotopography across the Northern Sicily Continental Margin (NSCM) and an overlying Zanclean m…

2018

During the Messinian salinity crisis (MSC) (from 5.97 to 5.33 Ma), the Mediterranean Sea became disconnected from the world’s oceans and a fast and continuous evaporation resulted in its partial desiccation. One of the theories for the end of the MSC postulates that a large volume of Atlantic waters entered the Mediterranean Sea through the Gibraltar Strait and rapidly refilled the Mediterranean basin in an event welldocumented known as the Zanclean Flood. The pathway of the Zanclean flood during its passage from the western to the eastern Mediterranean Sea is unclear. The aim of this study is to understand the effects of the Messinian palaeotopography of the southern Tyrrhenian Sea on the …

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaMessinian paleo-topography Zanclean flood Mass Transport Deposits.Settore GEO/03 - Geologia Strutturale
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The end of the Messinian salinity crisis: new insights from the Chelif Basin (Algeria)

2006

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaMessinian salinity crisiAlgeriaSettore GEO/01 - Paleontologia E Paleoecologia
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ORIGIN AND EVOLUTION OF THE MESSINIAN BASINS DEVELOPED ON TOP OF THE SICILIAN FOLD AND THRUST BELT

2016

During the Messinian the inherited paleo-topography conditioned the depositional environments of the Mediterranean region, already strongly influenced by the effects of the salinity crisis, mainly in the central region, where seabed at that time is expected to be very uneven and shallower than Western and Eastern Mediterranean. Indeed in this area as from 15 Ma the Sicilian Fold and Thrust Belt (SFTB) was originating, characterized by a multi-stage evolution: two main shortening events generated and developed at different structural levels (shallow- and deep-seated thrusts in thin-skinned thrust-model) and at different time intervals, involving mainly the Meso-Cenozoic carbonate units of th…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaMessinianGypsumThrust-top-Basin
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Paleoenvironmental changes at the Messinian/Pliocene boundary in the Alboran Area: The example of the Melilla Basin, NE Marocco

2004

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/01 - Paleontologia E PaleoecologiaMessinian-Pliocene boundary Marocco
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Basins at convergent margins: evolution of the Messinian basins developed on top of the Sicilian Fold and Thrust belt

2018

During the Messinian inherited palaeo-topography and ongoing deformation conditioned the depositional environments of the Mediterranean region, already strongly influenced by the effects of the salinity crisis. It occurred mainly in the central region, where seabed at that time is expected to be very uneven and shallower than Western and Eastern Mediterranean. Indeed in this area as from 15 Ma the Sicilian Fold and Thrust Belt (SFTB) was originating, characterized by a multi-stage evolution. Two main shortening events generated and developed at different structural levels (shallow- and deep-seated thrusts following a thin-skinned thrust-model) and at different time intervals, involved mainl…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleMessinian Syntectonic Basin Fold and Thrust Belt
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The Messinian Salinity Crisis in the Mediterranean: an integrated scenario

2004

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicamessinian salinity crisis mediterranean areaSettore GEO/01 - Paleontologia E Paleoecologia
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