Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Alvaro Rubio Ordoñez"'
Publikováno v:
Espacio, Tiempo y Forma. Serie I, Prehistoria y Arqueología, Iss 16, Pp 83-109 (2023)
This paper summarises the results of the first analytical investigation of the soil chemistry of Asturian Megalithism, an approach which is essential, due to the scarcity of materials conserved in the burial areas. The combination of three analytical
Externí odkaz:
https://doaj.org/article/70beb34711d347e48aad79d65ab59c7e
Autor:
Francisco José Fernández Rodríguez, Javier Escuder-Viruete, Fernando Pérez Valera, Pablo Valverde Vaquero, Mercedes Castillo Carrión, Álvaro Rubio Ordóñez, Alicia Medialdea
Publikováno v:
Geogaceta, Vol 74 (2023)
Las zonas de fallas de desgarre izquierdo de la cresta de Beata (BR) y derecho de Ocoa-Bonao-La-Guácara (OB) transfieren la deformación Plio-Cuaternaria que produce la indentación NNE del escarpe oceánico de Beata bajo el margen meridional de la
Externí odkaz:
https://doaj.org/article/2833d14832e644bdacc8c17d774bd829
Autor:
Javier Escuder-Viruete, Mercedes Castillo Carrión, Álvaro Rubio Ordóñez, Francisco José Fernández, Fernando Pérez Valera, Pablo Valverde Vaquero
Publikováno v:
Geogaceta, Vol 74 (2023)
Las diferencias texturales, químico-mineralógicas y en la orientación de la fábrica en la peridotita de Loma Caribe (PLC) permiten distinguir peridotitas granulares (PG) y porfiroclásticas (PPC). Las PG presentan foliaciones dúctiles de alta-T
Externí odkaz:
https://doaj.org/article/6abe9263ebd74f6ea3deeeebb49f4fee
Publikováno v:
International Journal of Earth Sciences. 100:1533-1550
The Nisa-Alburquerque granitic batholith (southern Variscan Belt, Iberian Peninsula) has been studied by petrological, structural and geophysical approaches, obtaining contrasting models for its deep structure and emplacement sequence. In order to te
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6d12c3493e99c935955848f9fdb355df
https://doi.org/10.1007/s00531-010-0568-4
https://doi.org/10.1007/s00531-010-0568-4
Publikováno v:
Talanta. 114
The historical Madrid meteorite chondrite fell in 1896 showing thin melt veins with a 65% of brecciated forsterite fragments surrounded by a fine grained matrix formed by troilite, chromite and Fe–Ni blebs. It exhibits a delicate iron infill, neo-f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a8f0be17c34add043b85a3de98c01ffe
https://pubmed.ncbi.nlm.nih.gov/23953455
https://pubmed.ncbi.nlm.nih.gov/23953455