Zobrazeno 1 - 10
of 12
pro vyhledávání: '"J. I. Gil-Ibarguchi"'
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:
B. Puente-Berdasco, J. Rodríguez, D. Ballesteros, A. Painchault, C. Nehme, D. Mouralis, J. I. Gil-Ibarguchi, A. Martín-Izard, J. I. Garcia Alonso
Publikováno v:
Journal of Analytical Atomic Spectrometry
Journal of Analytical Atomic Spectrometry, Royal Society of Chemistry, 2022, 37 (1), pp.194-202. ⟨10.1039/D1JA00340B⟩
Journal of Analytical Atomic Spectrometry, Royal Society of Chemistry, 2022, 37 (1), pp.194-202. ⟨10.1039/D1JA00340B⟩
International audience; A procedure for the measurement of 87Sr/86Sr in carbonates without off-line strontium separation was developed, validated and applied to Normandy chalkstones. The method is based on the injection of the dissolved/leached sampl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::857cb12f9e03e4df5b08c2800a0edbf7
https://halshs.archives-ouvertes.fr/halshs-03513240
https://halshs.archives-ouvertes.fr/halshs-03513240
Publikováno v:
Estudios Geologicos, Vol 70, Iss 2, Pp e012-e012 (2014)
El volcán Las Herrerías (Bolaños de Calatrava; Región Volcánica del Campo de Calatrava) se caracteriza por una gran cantidad y variedad de depósitos originados a partir de fuentes de lava. Todos estos depósitos son composicionalmente idéntico
Externí odkaz:
https://doaj.org/article/d264cc4a00db4fb1b50f80c9bdda721f
Publikováno v:
The Journal of Geology. 117:71-87
Amphibolite bodies with eclogite relics are interlayered at different levels in the Ojen nappe (Alpujarride Complex) below the Ronda peridotites of the Betic Cordilleras in southern Spain. We present an integrated structural, petrological, and geoche
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b19e203ad55aebb1a4e3b171159545db
https://doi.org/10.1086/593322
https://doi.org/10.1086/593322
Autor:
J. I. Gil Ibarguchi, M. Julivert
Publikováno v:
Estudios Geologicos, Vol 44, Iss 5-6, Pp 353-374 (1988)
Los materiales Paleozoicos que afloran en la Sierra de Collcerola (Tibidabo) van desde términos altos del Ordovíco hasta el Carbonífero. Estos Materiales se disponen aproximadamente en una estructura sinclinal con pliegues menores vergentes al SE
Externí odkaz:
https://doaj.org/article/c109ba7b3d0245bb820087da1e2a994d
Autor:
J. I. Gil Ibarguchi, J. M. Tubía
Publikováno v:
Journal of the Geological Society. 148:801-804
Eclogites interlayered with amphibolites and migmatites occur in an upper unit (OjCn nappe) of the Alpujarride complex (Betic Cor- dilleras). Estimates of P-T conditions reveal a retrograde meta-morphic path from an edogitic stage at >15 kbar and c.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a48f51ca1f616bc1026ab04d1966ef0
https://doi.org/10.1144/gsjgs.148.5.0801
https://doi.org/10.1144/gsjgs.148.5.0801
Publikováno v:
Pre-Mesozoic Geology of Iberia ISBN: 9783642839825
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa0485126bd06d222a54f16cf96c1e7b
https://doi.org/10.1007/978-3-642-83980-1_15
https://doi.org/10.1007/978-3-642-83980-1_15
Publikováno v:
Contributions to Mineralogy and Petrology. 80:14-24
The core of the El Tormes thermal dome, situated in the central part of one of the main metamorphic belts of the Iberian Peninsula, is formed by garnet-cordierite-biotite-sillimanite pelitic gneisses. These rocks, that very often are cut by minor int
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eb5a4c1448e571c34d03248ecb7a29f0
https://doi.org/10.1007/bf00376731
https://doi.org/10.1007/bf00376731
Autor:
E.Ortega Gironés, J. I. Gil Ibarguchi
Publikováno v:
Chemical Geology. 50:145-162
The Malpica—Tuy (MT) unit is a narrow band of basement in Galicia (northwest Spain) composed of mica schists, paragneisses and calc-alkaline to peralkaline orthogneisses with minor amounts of metamorphosed basic rocks. Garnet, omphacite, glaucophan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::672b232ad31f4b97933352ee48fb169a
https://doi.org/10.1016/0009-2541(85)90117-2
https://doi.org/10.1016/0009-2541(85)90117-2
Publikováno v:
The Journal of Geology. 92:397-416
Two series of granitoids are present in the Finisterre region. One is formed mainly by syn-collision two-mica leucogranites. The other is composed of syn- and post-collision granodiorites and monzogranites of calc-alkaline affinity. The emplacement o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3618555f3430dba482708ef0930d6c5c
https://doi.org/10.1086/628875
https://doi.org/10.1086/628875