Role of inheritance during tectonic inversion of a rift system in basement-involved to salt-decoupled transition: analogue modelling and application to the Pyrenean–Biscay system Article Swipe
Jordi Miró
,
Oriol Ferrer
,
Josep Antón Muñoz
,
Gianreto Manastchal
·
YOU?
·
· 2023
· Open Access
·
· DOI: https://doi.org/10.5194/se-14-425-2023
YOU?
·
· 2023
· Open Access
·
· DOI: https://doi.org/10.5194/se-14-425-2023
The reactivation of former rift systems and passive margins during tectonic inversion and their incorporation into fold-and-thrust belts result in significant structural differences not only between internal and external domains, but also along-strike. The Basque–Cantabrian and Asturian systems are among the best examples to address the role of along-strike changes in rift inheritance since they show a transition from salt to basement-inherited structures divided by a transition zone separating thick- from thin-skinned structural domains. While both domains have been widely described in the literature, the transfer system separating the two has not been sufficiently investigated due to poor seismic imaging and the lack of large-scale outcrops. This contribution aims to address the linkage between basement-controlled (i.e. thick-skinned) and salt-decoupled (i.e. thin-skinned) domains and to describe how deformation is accommodated in the transitional zone between these domains. An experimental programme based on analogue models has been designed that was inspired by the transition from the thin-skinned Basque–Cantabrian Pyrenees to the east to the thick-skinned Asturian Massif to the west. As observed in nature, experimental results show that oblique structures (at low angle with the shortening direction) form in the transitional domain, and their location depends on the linkage of the active structures occurring in both surrounding thick- and thin-skinned domains at different positions. Nevertheless, their orientation and evolution are controlled by the underlying decoupling horizon (i.e. salt). The deformation in the thick-skinned domain produces significant topography over a narrow deformation area due to the lack of effective decoupling levels. On the contrary, deformation in the thin-skinned domain is more distributed due to decoupling, resulting in a wider deformation area of less topography. As a result, syn-contractional sedimentation occurs mainly in the foreland basin in front of the thick-skinned domain, whereas it is observed in the foreland but also in piggyback basins in the thin-skinned domain.
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- Type
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- Language
- en
- Landing Page
- https://doi.org/10.5194/se-14-425-2023
- https://se.copernicus.org/articles/14/425/2023/se-14-425-2023.pdf
- OA Status
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- Cited By
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- References
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- Related Works
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- OpenAlex ID
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Raw OpenAlex JSON
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https://openalex.org/W4366771696Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.5194/se-14-425-2023Digital Object Identifier
- Title
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Role of inheritance during tectonic inversion of a rift system in basement-involved to salt-decoupled transition: analogue modelling and application to the Pyrenean–Biscay systemWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2023Year of publication
- Publication date
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2023-04-21Full publication date if available
- Authors
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Jordi Miró, Oriol Ferrer, Josep Antón Muñoz, Gianreto ManastchalList of authors in order
- Landing page
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https://doi.org/10.5194/se-14-425-2023Publisher landing page
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https://se.copernicus.org/articles/14/425/2023/se-14-425-2023.pdfDirect link to full text PDF
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goldOpen access status per OpenAlex
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https://se.copernicus.org/articles/14/425/2023/se-14-425-2023.pdfDirect OA link when available
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Geology, Rift, Massif, Tectonics, Salt tectonics, Inversion (geology), Paleontology, Oblique case, Seismology, Geometry, Petrology, Diapir, Linguistics, Philosophy, MathematicsTop concepts (fields/topics) attached by OpenAlex
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11Total citation count in OpenAlex
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2025: 4, 2024: 6, 2023: 1Per-year citation counts (last 5 years)
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10Other works algorithmically related by OpenAlex
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