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The importance of sequential partial melting and fractional crystallization in the generation of syn‑D3 Variscan two‑mica granites from the Carrazeda de Ansiães area, northern Portugal
dc.contributor.author | Teixeira, R. J. S. | |
dc.contributor.author | Neiva, A. M. R. | |
dc.contributor.author | Gomes, M. E. P. | |
dc.contributor.author | Corfu, F. | |
dc.contributor.author | Cuesta Fernández, Andrés | |
dc.contributor.author | Croudace, I. W. | |
dc.date.accessioned | 2021-02-25T13:20:14Z | |
dc.date.available | 2021-02-25T13:20:14Z | |
dc.date.issued | 2020 | |
dc.identifier.citation | Journal of Iberian Geology (2020); doi:10.1007/s41513-020-00160-x | |
dc.identifier.issn | 1698-6180 | |
dc.identifier.issn | 1886-7995 | |
dc.identifier.uri | http://hdl.handle.net/10651/58061 | |
dc.description.sponsorship | Funding was provided to R. J. S. Teixeira by the SFRH/BD/17246/2004 PhD Grant from FCT—Fundação para a Ciência e a Tecnologia, Portugal, and another grant from SOCFAC (Southampton Oceanography Centre, Facilities and Co-Operation). This research was financially supported by the Pole of the Geosciences Centre (CGeo) and projects UIDB/00073/2020 and UIDP/00073/2020 through FCT—Portuguese Foundation for Sciences and Technology. | spa |
dc.language.iso | eng | spa |
dc.relation.ispartof | Journal of Iberian Geology | spa |
dc.rights | © 2021, Universidad Complutense de Madrid | |
dc.rights | Esta versión del artículo ha sido aceptada para su publicación, después de la revisión por pares (cuando corresponda) y está sujeta a los términos de uso de AM de Springer Nature , pero no es la versión de registro y no refleja mejoras posteriores a la aceptación ni correcciones. La versión del registro está disponible en línea en: http://dx.doi.org/10.1007/s41513-020-00160-x | |
dc.rights | CC Reconocimiento - No comercial - Sin obras derivadas 4.0 Internacional | |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/4.0/ | |
dc.title | The importance of sequential partial melting and fractional crystallization in the generation of syn‑D3 Variscan two‑mica granites from the Carrazeda de Ansiães area, northern Portugal | spa |
dc.type | journal article | spa |
dc.identifier.doi | 10.1007/s41513-020-00160-x | |
dc.relation.publisherversion | http://dx.doi.org/10.1007/s41513-020-00160-x | spa |
dc.rights.accessRights | open access | |
dc.type.hasVersion | AM |