RAPPORTI FRA I PRODOTTI RESIDUALI DEL CARSISMO E LA SEDIMENTAZIONE QUATERNARIA NELL'AREA DELLE MURGE

The presence of red clays and silts, alternated with micritic limestones in the lower part of the Calcarenite di Gravina Formation (Lower Pleistocene) proves that, in some zones of the Murge area, the sedimentation was affected by residual materials coming from dissolution of Cretaceous limestones....

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Main Author: ANTONIA IANNONE
Format: Article
Language:English
Published: Milano University Press 2023-05-01
Series:Rivista Italiana di Paleontologia e Stratigrafia
Subjects:
Online Access:https://riviste.unimi.it/index.php/RIPS/article/view/20172
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author ANTONIA IANNONE
author_facet ANTONIA IANNONE
author_sort ANTONIA IANNONE
collection DOAJ
description The presence of red clays and silts, alternated with micritic limestones in the lower part of the Calcarenite di Gravina Formation (Lower Pleistocene) proves that, in some zones of the Murge area, the sedimentation was affected by residual materials coming from dissolution of Cretaceous limestones. The stratigraphyc data concerning the whole formation indicate that these environmental conditions took piace at the beginning of the pliopleistocenic transgression only; i, e. until the residual materials, produced and amassed by karst on the Murge area, reached the basin. The presedimentary morphotectonic setting was also of gecat importance: the presence of some hollows, prehexisting to the transgression, favoured the accumulation and the preservation of murgian terrigenous materials, which in other areas were removed by the sea action.
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spelling doaj.art-5034a5d6d9a141feb55c9c9bd7b3ee9e2023-09-03T13:19:02ZengMilano University PressRivista Italiana di Paleontologia e Stratigrafia0035-68832039-49422023-05-01882RAPPORTI FRA I PRODOTTI RESIDUALI DEL CARSISMO E LA SEDIMENTAZIONE QUATERNARIA NELL'AREA DELLE MURGE ANTONIA IANNONE The presence of red clays and silts, alternated with micritic limestones in the lower part of the Calcarenite di Gravina Formation (Lower Pleistocene) proves that, in some zones of the Murge area, the sedimentation was affected by residual materials coming from dissolution of Cretaceous limestones. The stratigraphyc data concerning the whole formation indicate that these environmental conditions took piace at the beginning of the pliopleistocenic transgression only; i, e. until the residual materials, produced and amassed by karst on the Murge area, reached the basin. The presedimentary morphotectonic setting was also of gecat importance: the presence of some hollows, prehexisting to the transgression, favoured the accumulation and the preservation of murgian terrigenous materials, which in other areas were removed by the sea action. https://riviste.unimi.it/index.php/RIPS/article/view/20172Karst; Quaternary sedimentation; South ltaly.
spellingShingle ANTONIA IANNONE
RAPPORTI FRA I PRODOTTI RESIDUALI DEL CARSISMO E LA SEDIMENTAZIONE QUATERNARIA NELL'AREA DELLE MURGE
Rivista Italiana di Paleontologia e Stratigrafia
Karst; Quaternary sedimentation; South ltaly.
title RAPPORTI FRA I PRODOTTI RESIDUALI DEL CARSISMO E LA SEDIMENTAZIONE QUATERNARIA NELL'AREA DELLE MURGE
title_full RAPPORTI FRA I PRODOTTI RESIDUALI DEL CARSISMO E LA SEDIMENTAZIONE QUATERNARIA NELL'AREA DELLE MURGE
title_fullStr RAPPORTI FRA I PRODOTTI RESIDUALI DEL CARSISMO E LA SEDIMENTAZIONE QUATERNARIA NELL'AREA DELLE MURGE
title_full_unstemmed RAPPORTI FRA I PRODOTTI RESIDUALI DEL CARSISMO E LA SEDIMENTAZIONE QUATERNARIA NELL'AREA DELLE MURGE
title_short RAPPORTI FRA I PRODOTTI RESIDUALI DEL CARSISMO E LA SEDIMENTAZIONE QUATERNARIA NELL'AREA DELLE MURGE
title_sort rapporti fra i prodotti residuali del carsismo e la sedimentazione quaternaria nell area delle murge
topic Karst; Quaternary sedimentation; South ltaly.
url https://riviste.unimi.it/index.php/RIPS/article/view/20172
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