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Publication details

Document type
Journal articles

Document subtype
Full paper

Title
Mississippian olistostromes of Iberia revisited: tectonic drivers of synorogenic carbonate platform/reef destruction

Participants in the publication
Ícaro Dias da Silva (Author)
Dep. Geologia
IDL
Manuel Francisco Pereira (Author)
UNIVERSIDADE DE ÉVORA
Emílio González Clavijo (Author)
José Brandão Silva (Author)
Instituto Dom Luiz (IDL), Faculdade de Ciências, Universidade de Lisboa, Campo Grande, 1749–016, Lisboa, Portugal

Summary
This paper reviews the synorogenic basins formed on the Gondwana side of the Variscan Orogen of Iberia, highlighting the widespread occurrence of calciturbiditic formations and olistostromes containing reef limestone olistoliths in Iberia's Variscan basins. Using key examples from the Variscan Orogen for comparison (the Azrou–Khenifra and Rhenohercynian basins), the significance of these olistostromes and flyschoid deposits is discussed. Our tectonic models of the Variscan belt in Iberia propose possible drivers of synorogenic carbonate platform/reef destruction responsible for the origin of calciturbidites and olistostromes. One model proposes the formation of an orogenic plateau via the lateral flow of partially molten orogenic roots in the context of Laurussia–Gondwana convergence following the destruction of the Rheic Ocean and slab retreat of the Gondwana (lower) plate. An alternative model invokes subduction of Palaeotethys oceanic lithosphere beneath the Gondwana (upper) plate. Both emphasize the Mississippian occurrence of a significant thermal anomaly beneath Gondwana that favoured strong lithosphere thinning, creating ideal conditions for synorogenic carbonate platform/reef destruction and the formation of calciturbidite deposits and olistostromes in Iberia. The Variscan palaeotopography would look similar in both situations. Distinguishing between these models is therefore not straightforward, with differences in the kinematics of regional tectonic transport in the superstructure of Mississippian gneiss domes.

Date of Publication
2024-02-09

Where published
Journal of the Geological Society

Publication Identifiers
ISSN - 0016-7649
eISSN - 2041-479X

Publisher
Geological Society of London

Volume
181
Number
2

Document Identifiers
DOI - https://doi.org/10.1144/jgs2023-187
URL - http://dx.doi.org/10.1144/jgs2023-187

Rankings
SCIMAGO Q1 (2022) - 1.122 - Geology

Keywords
Variscan Orogen Mississippian Synorogenic basins Oliostostromes

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APA
Ícaro Dias da Silva, Manuel Francisco Pereira, Emílio González Clavijo, José Brandão Silva, (2024). Mississippian olistostromes of Iberia revisited: tectonic drivers of synorogenic carbonate platform/reef destruction. Journal of the Geological Society, 181, ISSN 0016-7649. eISSN 2041-479X. http://dx.doi.org/10.1144/jgs2023-187

IEEE
Ícaro Dias da Silva, Manuel Francisco Pereira, Emílio González Clavijo, José Brandão Silva, "Mississippian olistostromes of Iberia revisited: tectonic drivers of synorogenic carbonate platform/reef destruction" in Journal of the Geological Society, vol. 181, 2024. 10.1144/jgs2023-187

BIBTEX
@article{60475, author = {Ícaro Dias da Silva and Manuel Francisco Pereira and Emílio González Clavijo and José Brandão Silva}, title = {Mississippian olistostromes of Iberia revisited: tectonic drivers of synorogenic carbonate platform/reef destruction}, journal = {Journal of the Geological Society}, year = 2024, volume = 181 }