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Geochemistry of the Baixo Alentejo Flysch Group, South Portuguese Zone: implications for provenance and palaeoweathering

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dc.contributor.authorFernandes, Paulo
dc.contributor.authorJorge, R. C. G. S.
dc.contributor.authorPereira, Zélia
dc.contributor.authorOliveira, José Tomás
dc.date.accessioned2014-09-25T13:14:34Z
dc.date.available2014-09-25T13:14:34Z
dc.date.issued2008
dc.date.updated2014-09-23T08:41:13Z
dc.description.abstractThe Baixo Alentejo Flysch Group (BAFG) is one of the domains of the South Portuguese Zone, consisting of deepwater tubiditic sediments, with more than 5 km in thickness. Stratigraphically the BAFG is subdivided into three formations, from the bottom to the top: Mértola Formation, Mira Formation and Brejeira Formation, with ages ranging from Middle to Upper Carboniferous.por
dc.identifier.citationFernandes, Paulo; Jorge, R.C.G.S.; Pereira, Zélia; Oliveira, José Tomás. Geochemistry of the Baixo Alentejo Flysch Group, South Portuguese Zone: Implications for provenance and palaeoweathering, Trabalho apresentado em Goldschmidt Conference, In Geochimica Cosmochimica Acta, Vancouver, 2008.por
dc.identifier.otherAUT: PFE01874;
dc.identifier.urihttp://hdl.handle.net/10400.1/5123
dc.language.isoporpor
dc.peerreviewednopor
dc.titleGeochemistry of the Baixo Alentejo Flysch Group, South Portuguese Zone: implications for provenance and palaeoweatheringpor
dc.typeconference object
dspace.entity.typePublication
oaire.citation.conferencePlaceVancouverpor
oaire.citation.endPage264por
oaire.citation.startPage264por
oaire.citation.titleGoldschmidt Conference Abstracts 2008por
person.familyNameFernandes
person.givenNamePaulo
person.identifier422469
person.identifier.ciencia-id051D-A133-65D9
person.identifier.orcid0000-0003-4888-0230
person.identifier.ridJ-6577-2014
person.identifier.scopus-author-id57197129025
rcaap.rightsopenAccesspor
rcaap.typeconferenceObjectpor
relation.isAuthorOfPublicationa2d98df3-a9c2-4364-a737-25b4e89df80b
relation.isAuthorOfPublication.latestForDiscoverya2d98df3-a9c2-4364-a737-25b4e89df80b

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