Forebulge migration in the foreland basin system of the central‐southern Apennine fold‐thrust belt (Italy): New high‐resolution Sr‐isotope dating constraints Article Swipe
Monia Sabbatino
,
Stefano Tavani
,
Stefano Vitale
,
Kei Ogata
,
Amerigo Corradetti
,
Lorenzo Consorti
,
Ilenia Arienzo
,
Anna Cipriani
,
Mariano Parente
·
YOU?
·
· 2021
· Open Access
·
· DOI: https://doi.org/10.1111/bre.12587
YOU?
·
· 2021
· Open Access
·
· DOI: https://doi.org/10.1111/bre.12587
The Apennines are a retreating collisional belt where the foreland basin system, across large domains, is floored by a subaerial forebulge unconformity developed due to forebulge uplift and erosion. This unconformity is overlain by a diachronous sequence of three lithostratigraphic units made of (a) shallow‐water carbonates, (b) hemipelagic marls and shales and (c) siliciclastic turbidites. Typically, the latter two have been interpreted regionally as the onset of syn‐orogenic deposition in the foredeep depozone, whereas little attention has been given to the underlying unit. Accordingly, the rate of migration of the central‐southern Apennine fold‐thrust belt‐foreland basin system has been constrained, so far, exclusively considering the age of the hemipelagites and turbidites, which largely post‐date the onset of foredeep depozone. In this work, we provide new high‐resolution ages obtained by strontium isotope stratigraphy applied to calcitic bivalve shells sampled at the base of the first syn‐orogenic deposits overlying the Eocene‐Cretaceous pre‐orogenic substratum. Integration of our results with published data indicates progressive rejuvenation of the strata sealing the forebulge unconformity towards the outer portions of the fold‐thrust belt. In particular, the age of the forebulge unconformity linearly scales with the pre‐orogenic position of the analysed sites, pointing to an overall constant migration velocity of the forebulge wave in the last 25 Myr.
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- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1111/bre.12587
- https://onlinelibrary.wiley.com/doi/pdfdirect/10.1111/bre.12587
- OA Status
- hybrid
- Cited By
- 24
- References
- 98
- Related Works
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- OpenAlex ID
- https://openalex.org/W3185070204
All OpenAlex metadata
Raw OpenAlex JSON
- OpenAlex ID
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https://openalex.org/W3185070204Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.1111/bre.12587Digital Object Identifier
- Title
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Forebulge migration in the foreland basin system of the central‐southern Apennine fold‐thrust belt (Italy): New high‐resolution Sr‐isotope dating constraintsWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2021Year of publication
- Publication date
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2021-07-16Full publication date if available
- Authors
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Monia Sabbatino, Stefano Tavani, Stefano Vitale, Kei Ogata, Amerigo Corradetti, Lorenzo Consorti, Ilenia Arienzo, Anna Cipriani, Mariano ParenteList of authors in order
- Landing page
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https://doi.org/10.1111/bre.12587Publisher landing page
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https://onlinelibrary.wiley.com/doi/pdfdirect/10.1111/bre.12587Direct link to full text PDF
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YesWhether a free full text is available
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hybridOpen access status per OpenAlex
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https://onlinelibrary.wiley.com/doi/pdfdirect/10.1111/bre.12587Direct OA link when available
- Concepts
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Foreland basin, Geology, Unconformity, Paleontology, Diachronous, Fold and thrust belt, Fold (higher-order function), Sedimentary rock, Structural basin, Engineering, Mechanical engineeringTop concepts (fields/topics) attached by OpenAlex
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24Total citation count in OpenAlex
- Citations by year (recent)
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2025: 4, 2024: 8, 2023: 4, 2022: 4, 2021: 4Per-year citation counts (last 5 years)
- References (count)
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98Number of works referenced by this work
- Related works (count)
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10Other works algorithmically related by OpenAlex
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