{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,2,28]],"date-time":"2026-02-28T07:04:54Z","timestamp":1772262294693,"version":"3.50.1"},"reference-count":96,"publisher":"Copernicus GmbH","issue":"4","license":[{"start":{"date-parts":[[2020,7,9]],"date-time":"2020-07-09T00:00:00Z","timestamp":1594252800000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100001871","name":"Funda\u00e7\u00e3o para a Ci\u00eancia e a Tecnologia","doi-asserted-by":"publisher","award":["SFRH\/BPD\/99550\/2014"],"award-info":[{"award-number":["SFRH\/BPD\/99550\/2014"]}],"id":[{"id":"10.13039\/501100001871","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Solid Earth"],"abstract":"<jats:p>Abstract. Carboniferous siliciclastic and silicic magmatic rocks from the\nSanta Susana\u2013S\u00e3o Cristov\u00e3o and Cabrela regions contain valuable\ninformation regarding the timing of synorogenic processes in SW Iberia. In\nthis region of the Ossa-Morena Zone (OMZ), late Carboniferous terrigenous\nstrata (i.e., the Santa Susana Formation) unconformably overlie early\nCarboniferous marine siliciclastic deposits alternating with volcanic rocks\n(i.e., the Toca da Moura volcano-sedimentary complex). Lying below this\nintra-Carboniferous unconformity, the Toca da Moura volcano-sedimentary\ncomplex is intruded and overlain by the Baleiz\u00e3o porphyry. Original\nsensitive high-resolution ion microprobe (SHRIMP) and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) U\u2013Pb zircon are presented in this paper, providing\nchronostratigraphic and provenance constraints since available\ngeochronological information is scarce and only biostratigraphic ages are\ncurrently available for the Santa Susana\u2013S\u00e3o Cristov\u00e3o region. Our\nfindings and the currently available detrital zircon ages from Paleozoic\nterranes of SW Iberia (Pulo do Lobo Zone \u2013 PLZ \u2013 South Portuguese Zone \u2013 SPZ \u2013 and OMZ) were jointly analyzed using the K\u2013S test and multidimensional scaling (MDS) diagrams to\ninvestigate provenance. The marine deposition is constrained to the age\nrange of ca. 335\u2013331\u2009Ma (Visean) by new U\u2013Pb data for silicic tuffs from the Toca da Moura and Cabrela volcano-sedimentary complexes. The\nBaleiz\u00e3o porphyry, intrusive in the Toca da Moura volcano-sedimentary\ncomplex, yielded a crystallization age of ca. 318\u2009Ma (Bashkirian), providing\nthe minimum age for the overlying intra-Carboniferous unconformity. A\ncomparison of detrital zircon populations from siliciclastic rocks of the\nCabrela and Toca de Moura volcano-sedimentary complexes of the OMZ suggests\nthat they are derived from distinct sources more closely associated with the SPZ\nand PLZ than the OMZ. Above the intra-Carboniferous unconformity, the Santa\nSusana Formation is the result of the recycling of distinct sources\nlocated either on the Laurussian side (SPZ and PLZ) or Gondwanan side (OMZ) of the\nRheic suture zone. The best estimate of the crystallization age of a granite\ncobble which was found in a conglomerate from the Santa Susana Formation yielded ca. 303\u2009Ma (Kasimovian\u2013Gzhelian), representing the maximum depositional age for\nthe terrestrial strata. The intra-Carboniferous unconformity seems to\nrepresent a stratigraphic gap of approximately 12\u201314\u2009Myr, providing evidence\nof the rapid post-accretion and collision uplift of the Variscan orogenic belt\nin SW Iberia (i.e., the OMZ, PLZ, and SPZ).<\/jats:p>","DOI":"10.5194\/se-11-1291-2020","type":"journal-article","created":{"date-parts":[[2020,7,9]],"date-time":"2020-07-09T01:35:02Z","timestamp":1594258502000},"page":"1291-1312","source":"Crossref","is-referenced-by-count":15,"title":["Chronostratigraphic framework and provenance of the Ossa-Morena Zone Carboniferous basins (southwest Iberia)"],"prefix":"10.5194","volume":"11","author":[{"given":"Manuel Francisco","family":"Pereira","sequence":"first","affiliation":[]},{"given":"Cristina","family":"Gama","sequence":"additional","affiliation":[]},{"given":"\u00cdcaro","family":"Dias da Silva","sequence":"additional","affiliation":[]},{"given":"Jos\u00e9 Brand\u00e3o","family":"Silva","sequence":"additional","affiliation":[]},{"given":"Mandy","family":"Hofmann","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0003-0970-0233","authenticated-orcid":false,"given":"Ulf","family":"Linnemann","sequence":"additional","affiliation":[]},{"ORCID":"https:\/\/orcid.org\/0000-0002-1670-7305","authenticated-orcid":false,"given":"Andreas","family":"G\u00e4rtner","sequence":"additional","affiliation":[]}],"member":"3145","published-online":{"date-parts":[[2020,7,9]]},"reference":[{"key":"ref1","unstructured":"Andrade, A. 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