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Studying in the Paxos Zone the Carbonate depositional enviroment changes during upper Cretaceous, in Sami area of Kefallinia Island, Greece
Studying in the Paxos Zone the Carbonate depositional enviroment changes during upper Cretaceous, in Sami area of Kefallinia Island, Greece
dc.date.accessioned:
2021-08-02T20:40:42Z
dc.date.available: 2021-08-02T20:40:42Z
dc.date.issued: 2010-05
dc.identifier.uri: http://ermis.di.ionio.gr/xmlui/handle/123456789/1144
dc.description: The shallow-marine carbonate sequence of Sami is a part of the Upper Cretaceous carbonate platform of the Paxi zone. Detailed lithostratigraphic and microfacies analysis of that sequence revealed clear periodicities and cyclicity. The high-resolution stratigraphic analysis has shown a number of lithofacies organized in groups (lithofacies associations), suggesting, on the whole, sedimentary environments ranging from lagoonal to peritidal context. The vertical arrangement of these lithofacies allowed the identification of a cyclic recurrence of the depositional and early diagenetic features, including a meteoric overprint on top of the elementary cycles. The cycles exhibit a shallowing upward trend from shallow subtidal to inter-supratidal and hypersaline facies, in a warm shallow marine environment.
dc.language.iso: en
dc.subject: Geology
dc.subject: Upper Cretaceous
dc.subject: Paxi Zone
dc.subject: Kefalonia
dc.title: Studying in the Paxos Zone the Carbonate depositional enviroment changes during upper Cretaceous, in Sami area of Kefallinia Island, Greece
dc.type: Working Paper
dc.date.available: 2021-08-02T20:40:42Z
dc.date.issued: 2010-05
dc.identifier.uri: http://ermis.di.ionio.gr/xmlui/handle/123456789/1144
dc.description: The shallow-marine carbonate sequence of Sami is a part of the Upper Cretaceous carbonate platform of the Paxi zone. Detailed lithostratigraphic and microfacies analysis of that sequence revealed clear periodicities and cyclicity. The high-resolution stratigraphic analysis has shown a number of lithofacies organized in groups (lithofacies associations), suggesting, on the whole, sedimentary environments ranging from lagoonal to peritidal context. The vertical arrangement of these lithofacies allowed the identification of a cyclic recurrence of the depositional and early diagenetic features, including a meteoric overprint on top of the elementary cycles. The cycles exhibit a shallowing upward trend from shallow subtidal to inter-supratidal and hypersaline facies, in a warm shallow marine environment.
dc.language.iso: en
dc.subject: Geology
dc.subject: Upper Cretaceous
dc.subject: Paxi Zone
dc.subject: Kefalonia
dc.title: Studying in the Paxos Zone the Carbonate depositional enviroment changes during upper Cretaceous, in Sami area of Kefallinia Island, Greece
dc.type: Working Paper
The shallow-marine carbonate sequence of Sami is a part of the Upper Cretaceous carbonate platform of the Paxi zone. Detailed lithostratigraphic and microfacies analysis of that sequence revealed clear periodicities and cyclicity. The high-resolution stratigraphic analysis has shown a number of lithofacies organized in groups (lithofacies associations), suggesting, on the whole, sedimentary environments ranging from lagoonal to peritidal context. The vertical arrangement of these lithofacies allowed the identification of a cyclic recurrence of the depositional and early diagenetic features, including a meteoric overprint on top of the elementary cycles. The cycles exhibit a shallowing upward trend from shallow subtidal to inter-supratidal and hypersaline facies, in a warm shallow marine environment.
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