Search results for "Triassic"

showing 10 items of 117 documents

Detrital zircon and micropalaeontological ages as new constraints for the lowermost tectonic unit (Talea Ori unit) of Crete, Greece

2007

The Talea Ori unit is the lowermost known tectonic unit of Crete and the most external part of the Hellenides. Its stratigraphy ranges from Late Carboniferous to Oligocene and outcrops of the lower part are only known in the Talea Ori mountains (central Crete). In this area, a black sandstone at the base of the Galinos Beds, thought to be the oldest formation, contains zircons which were dated using the single grain evaporation method. The majority of these grains yielded Late Carboniferous ages (Variscan), while a small group yielded Early Proterozoic ages. The age distribution of these zircons suggests that, at the Carboniferous–Permian boundary, not much of the older North Gondwanan base…

RiftPermianProterozoicCarbonate platformEarly TriassicPaleontologyDetrital zirconForaminiferaPermianOceanographyCreteTriassicConglomeratePaleontologyBasement (geology)Carboniferousddc:550External HellenidesEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Upper Triassic-Jurassic carbonate Platform-Pelagic Plateau Systems From Western Sicily

2009

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate Platform Upper Triassic Jurassic Sicily
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Middle Triassic (Ladinian) deep-water sediments in Sicily: New findings from the Madonie Mountains

2012

A section of carbonate megabreccias grading upward to deep-water Daonella limestones is described from the locality of Sant’Otiero, near Petralia Sottana, in the Madonie Mountains (Sicily). The megabreccia mainly consists of neritic elements containing dasycladalean algae (Diplopora annulatissima Pia) along with benthic foraminifers and problematics. The overlying calcilutitic strata are characterized by lumachella intercalations containing the bivalve Daonella tyrolensis Mojsisovics suggesting an early Late Ladinian (Protrachyceras longobardicum ammonoid zone) age. We informally name the Daonella limestone as the calcare di Sant’Otiero (Sant’Otiero limestone). The Daonella limestones along…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaDaonellaStratigraphylcsh:QE1-996.5PaleontologyTriassicLadinianlcsh:Geologylcsh:PaleontologyDeep-water limestonesTriassic Ladinian Sicily Daonella deep-water limestones stratigraphy paleontologySicilylcsh:QE701-760Triassic; Ladinian; Sicily; Daonella; Deep-water limestones; Stratigraphy; Paleontology
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Triassic/Jurassic carbonates from Western Sicily: their facies and implications for the end-Triassic biotic crisis.

2008

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaJurassic Platform-basin transition Reef Sicily T/J boundary Triassic
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La sezione di Pizzo Sant'Otiero (Petralia Sottana - Madonie) Geosito peculiare per l'evoluzione medio-triassica dell'area Centro-Mediterranea

2014

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSant'Otiero Madonie Triassico Medio Panormide Sicilia
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Geological framework of Sicily and the Triassic-Jurassic stratigraphic evolution

2010

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaTRIASSICSICILYJURASSIC
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Middle Triassic carbonate platform-basin system from Sicily. New evidence from the Madonie Mountains

2012

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaTriassic Ladinian Sicily Diplopora Daonella
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The late Carnian Rhaetian Succession at Pizzo Mondello (Sicani Mountains).

2010

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaTriassic Sicily stratigraphy GSSP Carnian Norian Boundary
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Karstic overprint of Upper Triassic peritidal cycles: The example of the Panormide Carbonate Platform at San Vito lo Capo (Sicily)

2012

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaTriassic carbonate platform karstic dissolution carbonate porosity Sicily.
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Sedimentology and biostratigraphy of a peritidal succession across the Triassic/Jurassic boundary: Monte Sparagio, north western Sicily

2016

A 490 m thick section of shallowing upward peritidal cycles spanning the Triassic-Jurassic boundary is exposed along the northern slope of Mount Sparagio in the San Vito Lo Capo Peninsula (Western Sicily). A detailed microfacies analysis allowed defining the aspects of cyclic sedimentation of this section and especially the stratigraphic occurrence patterns of benthic foraminifera and algae across the T/J boundary. The lower part of cycles commonly shows medium to low energy subtidal facies, typical of the inner lagoon of the carbonate platform. Subtidal facies such as coral bafflestone in some cycles suggest more open lagoonal conditions (patch reefs), while some higher energy layers such …

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaTriassic-Jurassic boundary carbonate Platform biotic crises
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