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ALLOCYCLIC MECHANISM OF SEDIMENTATION: A CASE STUDY FROM THE LOWER SARMATIAN MARGINAL DEPOSITS OF THE EAST-SLOVAKIAN NEOGENE BASIN
The Lower Sarmatian deposits in the Košice area, located on the margin of the East-Slovakian Basin, are arranged into stacked, fining-upward cycles. Each cycle, bounded by transgressive erosional boundaries comprises deltaic deposits on the base passing upward into shoreface deposits capped by offshore-transition zone deposits. The facies successions indicate an overall transgressive trend during the deposition punctuated by short periods of emergence. The cyclicity was governed by theallocyclic mechanism with the main role of episodic uplift events of the hinterland. The transition of deltaic and shoreface deposits into offshore-transition facies within individual cycles records a rapid increasing of accommodation space suggesting both a sea level rise and a basin floor subsidence
ALLOCYCLIC MECHANISM OF SEDIMENTATION: A CASE STUDY FROM THE LOWER SARMATIAN MARGINAL DEPOSITS OF THE EAST-SLOVAKIAN NEOGENE BASIN
The Lower Sarmatian deposits in the Košice area, located on the margin of the East-Slovakian Basin, are arranged into stacked, fining-upward cycles. Each cycle, bounded by transgressive erosional boundaries comprises deltaic deposits on the base passing upward into shoreface deposits capped by offshore-transition zone deposits. The facies successions indicate an overall transgressive trend during the deposition punctuated by short periods of emergence. The cyclicity was governed by theallocyclic mechanism with the main role of episodic uplift events of the hinterland. The transition of deltaic and shoreface deposits into offshore-transition facies within individual cycles records a rapid increasing of accommodation space suggesting both a sea level rise and a basin floor subsidence
ALLOCYCLIC MECHANISM OF SEDIMENTATION: A CASE STUDY FROM THE LOWER SARMATIAN MARGINAL DEPOSITS OF THE EAST-SLOVAKIAN NEOGENE BASIN
Janočko Juraj (Autor:in)
1997
Aufsatz (Zeitschrift)
Elektronische Ressource
Unbekannt
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