Zobrazeno 1 - 10
of 53
pro vyhledávání: '"M. Carracedo-Sánchez"'
Autor:
F. Sarrionandia, J. Errandonea‐Martin, E. Larrondo, M. Carracedo‐Sánchez, B. Ábalos, J. I. Gil Ibarguchi
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 11, Pp n/a-n/a (2023)
Abstract In the Mississippian Matachel small volcanic field of the Ossa‐Morena Zone (southern Iberian Massif) outpoured basic‐intermediate lavas exhibit geochemical characteristics of Low‐Ti continental tholeiites and calc‐alkaline lavas. Low
Externí odkaz:
https://doaj.org/article/1fa4c0073f16485db084b7efec15fe3a
Autor:
F. Sarrionandia, J. Errandonea-Martin, E. Larrondo, M. Carracedo-Sánchez, B. Ábalos, J.I. Gil-Ibarguchi
Publikováno v:
Data in Brief, Vol 46, Iss , Pp 108826- (2023)
The Matachel Basin is a tectono-stratigraphic unit of Ossa-Morena Zone (southern Iberian Massif) that encompasses an Upper Tournaisian – Viséan basaltic sequence, generated by effusive and explosive eruptions in a shallow submarine setting. A coll
Externí odkaz:
https://doaj.org/article/be9a6438e3204046af025806e7ec07e3
Publikováno v:
Geologica Acta, Vol 16, Iss 3 (2018)
The Sierra Bermeja Pluton (southern Central Iberian Zone, Iberian Massif) is a late-Variscan intrusive constituted by cordierite-bearing peraluminous monzogranites. Detailed field mapping has allowed to disclose the presence of several NE–SW trendi
Externí odkaz:
https://doaj.org/article/7378296b9f564715ab2301df53d23e76
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:
F. Sarrionandia, J. Errandonea-Martin, E. Larrondo, M. Carracedo-Sánchez, B. Ábalos, J.I. Gil-Ibarguchi
Publikováno v:
Data in brief. 46
The Matachel Basin is a tectono-stratigraphic unit of Ossa-Morena Zone (southern Iberian Massif) that encompasses an Upper Tournaisian – Viséan basaltic sequence, generated by effusive and explosive eruptions in a shallow submarine setting. A coll
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::075f3ce020ffa4902f4d09d8da5115c9
https://pubmed.ncbi.nlm.nih.gov/36591386
https://pubmed.ncbi.nlm.nih.gov/36591386
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
Autor:
José Ignacio Gil Ibarguchi, J. Errandonea-Martin, F. Sarrionandia, Vojtěch Janoušek, M. Carracedo-Sánchez
Publikováno v:
Lithos. :440-462
Voluminous peraluminous (biotite, biotite–cordierite and cordierite–muscovite-bearing) granitic plutons were emplaced in the southern part of the Central Iberian Zone (Iberian Massif) during the waning stages of the Variscan Orogeny. The role of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::74cb8c37e223097cbdb1daf23eaff7a5
https://doi.org/10.1016/j.lithos.2019.06.009
https://doi.org/10.1016/j.lithos.2019.06.009
Publikováno v:
Geological Journal. 54:3509-3526
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ac490cb46c2bac2b32eca6ec0ef13e0d
https://doi.org/10.1002/gj.3342
https://doi.org/10.1002/gj.3342
Autor:
M. Carracedo-Sánchez, J. Errandonea-Martin, Benito Ábalos, J.I. Gil Ibarguchi, F. Sarrionandia
Publikováno v:
Journal of Volcanology and Geothermal Research. 348:82-95
The Manoteras volcano (Tortonian to Pleistocene, Calatrava Volcanic Field, Spain) is composed of a scoria and spatter cone surrounded by a field of pahoehoe lava. The volcanic cone is made essentially of vitreous lapilli-tuffs with intercalations of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75afe7c4688a479618c0480a20782562
https://doi.org/10.1016/j.jvolgeores.2017.10.014
https://doi.org/10.1016/j.jvolgeores.2017.10.014