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Contact metamorphism and dolomitization overprint on Cambrian carbonates from the Ossa‑Morena Zone (SW Iberian Massif): implications to Sr‑chronology of carbonate rocks

dc.contributor.authorRoseiro, José
dc.contributor.authorMoreira, Noel
dc.contributor.authorAndrade, Laura
dc.contributor.authorNogueira, Pedro
dc.contributor.authorde Oliveira, Daniel Pipa Soares
dc.contributor.authorEguiluz, Luis
dc.contributor.authorMirao, Jose
dc.contributor.authorMoita, Patrícia
dc.contributor.authorSantos, José Francisco
dc.contributor.authorRibeiro, Sara
dc.contributor.authorPedro, J.
dc.date.accessioned2024-11-15T16:19:56Z
dc.date.available2024-11-15T16:19:56Z
dc.date.issued2024-11
dc.description.abstractABSTRACT: he Cambrian Series 2 Carbonate Formation from the Alter do Chão Elvas-Cumbres Mayores unit (Ossa-Morena Zone, SW Iberian Massif) is composed of regionally metamorphosed marbles and marlstones that underwent chlorite zone metamorphism and preserve the primaeval limestone 87Sr/86Sr ratios (0.7083–0.7088). These are consistent with the established Lower Cambrian seawater curve, and therefore used for age constraints in formations lacking fossil contents. The regional mineralogical and Sr-isotopic features of the carbonate rocks are frequently overprinted by the effects of contact metamorphism induced by magmatic bodies emplaced during rift-related and synorogenic events of the Palaeozoic, as well as by post-metamorphic dolomitization processes. The development of calc-silicate minerals due to contact metamorphism is common in the rocks of the Carbonate Formation and apparently results from the interaction of the protolith with fluids of different origin: (i) internally produced fluids released by conductive heating (observed in external contact aureoles) and (ii) external intrusion-expelled fluids that, besides leading to the appearance of distinctive assemblages, also promote an influx of strontium content (observed in roof pendants). Calc-silicate mineralogy varies substantially throughout the region, likely due to the heterogeneous distribution of silicate minerals of the protolith, progression of intrusion-driven fluids, and the irregular effect of thermal gradients. Results suggest that high-grade contact metamorphism (hornblende facies or higher) and dolomitization processes imposed on the Carbonate Formation significantly influence the isotopic signatures of the carbonates, providing limitations in applying Sr-isotopic chronology.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationRoseiro, J., Moreira, N., Andrade, L., Nogueira, P., Oliveira, D., Eguiluz, L., Mirão, J., Moita, P., Santos, J.F., Ribeiro, S. & Pedro, J. (2024) Contact metamorphism and dolomitization overprint on Cambrian carbonates from the Ossa‑Morena Zone (SW Iberian Massif): implications to Sr‑chronology of carbonate rocks. In: International Journal of Earth Sciences (Geol Rundsch), 2024. https://doi.org/10.1007/s00531-024-02476-wpt_PT
dc.identifier.doi10.1007/s00531-024-02476-wpt_PT
dc.identifier.eissn1437-3262
dc.identifier.issn1437-3254
dc.identifier.urihttp://hdl.handle.net/10400.9/4384
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherSpringerpt_PT
dc.relationALT20-03-0145-FEDER-000028pt_PT
dc.relationFrom mantle to Iberia: crust-mantle interaction, geodynamic evolution and ore forming systems of alkaline melts in the northernmost Ossa-Morena Zone domains
dc.relationINSTITUTE OF EARTH SCIENCES
dc.relationINSTITUTE OF EARTH SCIENCES
dc.relationHERCULES Laboratory - Cultural Heritage, Studies and Safeguard
dc.relationHERCULES Laboratory - Cultural Heritage, Studies and Safeguard
dc.relationGeoBioSciences GeoTechnologies and GeoEngineering
dc.relation.publisherversionhttps://doi.org/10.1007/s00531-024-02476-wpt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectMineralogypt_PT
dc.subjectMetamorphismpt_PT
dc.subjectCambrian carbonatespt_PT
dc.subjectOssa-Morena Zonept_PT
dc.subjectIberian Massifpt_PT
dc.titleContact metamorphism and dolomitization overprint on Cambrian carbonates from the Ossa‑Morena Zone (SW Iberian Massif): implications to Sr‑chronology of carbonate rockspt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.awardTitleFrom mantle to Iberia: crust-mantle interaction, geodynamic evolution and ore forming systems of alkaline melts in the northernmost Ossa-Morena Zone domains
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oaire.citation.titleInternational Journal of Earth Sciencespt_PT
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