Zobrazeno 1 - 10
of 31
pro vyhledávání: '"S. GARCÍA DE MADINABEITIA"'
Autor:
J. ERRANDONEA-MARTÍN, M. CARRACEDO-SÁNCHEZ, F. SARRIONANDIA, J.F. SANTOS ZALDUEGUI, S. GARCÍA DE MADINABEITIA, J.I. GIL-IBARGUCHI
Publikováno v:
Geologica Acta, Vol 15, Iss 4 (2017)
The Valdepeñas pluton is the easternmost outcrop of the Cáceres-Valdepeñas magmatic alignment (southern Central Iberian Zone). This massif is constituted by a cordierite-bearing porphyritic monzogranite and may be grouped within the so-called “S
Externí odkaz:
https://doaj.org/article/faa5696a7fd046b39491d9260b56237b
Autor:
A. Beranoaguirre, B. Ábalos, S. García de Madinabeitia, J-L. Paquette, C. Pin, M.E. Sánchez Lorda, J.F. Santos Zalduegui, P. Puelles, J.I. Gil Ibarguchi
Publikováno v:
International Geology Review. :1-26
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31c2f8dcacaf76774280b89837868579
https://doi.org/10.1080/00206814.2022.2089923
https://doi.org/10.1080/00206814.2022.2089923
Akademický článek
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Autor:
P. Puelles, S. García de Madinabeitia, J.I. Gil Ibarguchi, M. Carracedo-Sánchez, S. Fernández-Armas, F. Sarrionandia
Publikováno v:
Lithos. :114-134
The microstructural, petrofabric and geochronological study of deep-seated xenoliths from the La Encomienda volcano (Neogene Campo de Calatrava Volcanic Field) has helped to characterize the nature and dynamics of processes operative in the lower cru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1da2f1554fa472975b26f2ce737e25dc
https://doi.org/10.1016/j.lithos.2019.05.031
https://doi.org/10.1016/j.lithos.2019.05.031
Publikováno v:
International Journal of Earth Sciences. 108:2037-2046
An isotopic resetting event is disclosed at ca. 350 Ma, based on Rb–Sr isotopic analyses (whole rock, garnet, clinopyroxene and phengite fractions) of eclogites with coronitic garnet and planolinear eclogites from the Malpica–Tui Allochthonous Co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5054cfdc6261361fa39bad8fed59b599
https://doi.org/10.1007/s00531-019-01747-1
https://doi.org/10.1007/s00531-019-01747-1
Publikováno v:
Addi. Archivo Digital para la Docencia y la Investigación
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[EN] Although sometimes controversial, the use of Pb isotope data in geological research of ore deposits and metal provenance studies in archaeology has proved a useful tool for investigation of the relations between ore sources and raw materials use
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::48f5d00766019d7c4688aa16f7419384
http://hdl.handle.net/10810/53768
http://hdl.handle.net/10810/53768
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
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K zobrazení výsledku je třeba se přihlásit.
Autor:
F. Sarrionandia, J.F. Santos-Zalduegui, J.I. Gil Ibarguchi, M. Carracedo-Sánchez, Benito Ábalos, J. Errandonea-Martin, S. García de Madinabeitia, L. Eguíluz
Publikováno v:
Lithos. :105765
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::67fc266215cfbec21a68d8c56abab048
https://doi.org/10.1016/j.lithos.2020.105765
https://doi.org/10.1016/j.lithos.2020.105765
Autor:
J.I. Gil Ibarguchi, M. E. Sánchez Lorda, A. Beranoaguirre, Benito Ábalos, S. García de Madinabeitia, P. Puelles
Publikováno v:
Lithos. :105660
Paired LA-ICP-MS U Pb and Lu Hf isotopic data and trace element data are reported on zircon in thin section from poorly known acid migmatites exposed in the Cabo Ortegal Complex, Western Variscides, NW Spain. The migmatites are part of the high-press
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6b3604efc8de318b5987b5f757983fc8
https://doi.org/10.1016/j.lithos.2020.105660
https://doi.org/10.1016/j.lithos.2020.105660
Autor:
L. Eguíluz, J. Errandonea-Martin, J.I. Gil Ibarguchi, M. Carracedo-Sánchez, F. Sarrionandia, S. García de Madinabeitia, J.F. Santos-Zalduegui, Benito Ábalos
Publikováno v:
Lithos. :105683
The Ossa-Morena Zone of the SW Iberian Massif encloses an arc-related assemblage ascribable to subduction processes that encompass the latest Cryogenian-early Cambrian. It started ca. 645 Ma ago and is recorded by coeval N-MORB and E-MORB type magmat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01326ef33845c809ae924a164caa865d
https://doi.org/10.1016/j.lithos.2020.105683
https://doi.org/10.1016/j.lithos.2020.105683