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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.<\/jats:p>\n          <jats:p>\n            <jats:bold>Graphical abstract<\/jats:bold>\n          <\/jats:p>","DOI":"10.1007\/s00531-024-02476-w","type":"journal-article","created":{"date-parts":[[2024,11,6]],"date-time":"2024-11-06T13:03:27Z","timestamp":1730898207000},"page":"193-217","update-policy":"https:\/\/doi.org\/10.1007\/springer_crossmark_policy","source":"Crossref","is-referenced-by-count":3,"title":["Contact metamorphism and dolomitization overprint on Cambrian carbonates from the Ossa-Morena Zone (SW Iberian Massif): implications to Sr-chronology of carbonate rocks"],"prefix":"10.1007","volume":"114","author":[{"ORCID":"https:\/\/orcid.org\/0000-0003-3643-9122","authenticated-orcid":false,"given":"Jos\u00e9","family":"Roseiro","sequence":"first","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0003-0415-1474","authenticated-orcid":false,"given":"Noel","family":"Moreira","sequence":"additional","affiliation":[]},{"given":"Laura","family":"Andrade","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0002-6162-0030","authenticated-orcid":false,"given":"Pedro","family":"Nogueira","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0002-6338-8845","authenticated-orcid":false,"given":"Daniel","family":"de Oliveira","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0002-2912-6403","authenticated-orcid":false,"given":"Luis","family":"Eguiluz","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0003-0103-3448","authenticated-orcid":false,"given":"Jos\u00e9","family":"Mir\u00e3o","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0001-9118-2249","authenticated-orcid":false,"given":"Patr\u00edcia","family":"Moita","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0003-4997-8264","authenticated-orcid":false,"given":"Jos\u00e9 Francisco","family":"Santos","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0002-5074-5452","authenticated-orcid":false,"given":"Sara","family":"Ribeiro","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0001-9376-5659","authenticated-orcid":false,"given":"Jorge","family":"Pedro","sequence":"additional","affiliation":[]}],"member":"297","published-online":{"date-parts":[[2024,11,6]]},"reference":[{"key":"2476_CR1","doi-asserted-by":"publisher","first-page":"113","DOI":"10.1016\/j.jafrearsci.2014.03.024","volume":"98","author":"JJ \u00c1lvaro","year":"2014","unstructured":"\u00c1lvaro JJ, Bellido F, Gasquet D, Pereira MF, Quesada C, S\u00e1nchez-Garc\u00eda T (2014) Diachronism in the late Neoproterozoic-Cambrian arc-rift transition of North Gondwana: a comparison of Morocco and the Iberian Ossa-Morena Zone. 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