Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Ana NEIRA CAMPOS"'
Autor:
M. Natividad Fuertes-Prieto, Esperanza Fernández-Martínez, Fernando Gómez-Fernández, Eduardo Alonso-Herrero, Diego Herrero Alonso, Ana Neira-Campos
Publikováno v:
Journal of Lithic Studies, Vol 3, Iss 2, Pp 309-326 (2016)
A study of the chert nodules found in the Escalada Formation (Carboniferous, Ponga region, Cantabrian Zone) was carried out as a means to characterise a number of lithic raw materials found in several prehistoric sites of the Cantabrian Mountains (NW
Externí odkaz:
https://doaj.org/article/b446d14de01e408aad615b9dd787dcef
Publikováno v:
Journal of Lithic Studies, Vol 3, Iss 2, Pp 389-410 (2016)
This work provides the keys to the mineralogical and geochemical characterization of black chert from the Vegamián Fm. This formation crops out throughout the whole of the Cantabrian Zone (of Palaeozoic age), one of the geological zones of the Canta
Externí odkaz:
https://doaj.org/article/a2216541c29540bd95ea722a3e347142
Autor:
M. Natividad Fuertes-Prieto, Ana Neira-Campos, Esperanza Fernández-Martínez, Fernando Gómez-Fernández, Eduardo Alonso-Herrero
Publikováno v:
Journal of Lithic Studies, Vol 1, Iss 1, Pp 117-135 (2014)
The so-called “Mucientes chert" is a variety that appears in the central area of the Iberian North Plateau, in theDueroBasin. It is widely known in the geological and archaeological literature and its use for knapping was especially important in Pr
Externí odkaz:
https://doaj.org/article/dd66fa30b0f442a48fdc37051bb28600
Publikováno v:
Lithic Technology. 46:236-257
The lithic operational chains at the Mesolithic site of La Una (Leon, N Spain) have been analysed and reconstructed through a joint study of the raw material provenance and technological characteri...
Autor:
Ana Neira Campos
Publikováno v:
Estudios humanísticos. Geografía, historia y arte. :145-154
This paper presents a revision of paleolithic research history in the province of Leon, from the firts scholars up to present time. Afterwards, it offers a brief state of current research in this province, showing their relationships with near geogra
Autor:
Ana Neira-Campos, Natividad Fuertes-Prieto, Esperanza Fernández-Martínez, Diego Herrero-Alonso, Antonio Tarriño-Vinagre
Publikováno v:
Archaeological and Anthropological Sciences. 13
The Cantabrian Zone (N of Spain) is characterized by an occurrence of Palaeozoic age materials, mainly belonging to the Devonian and Carboniferous. Among the different lithologies, certain facies contain black chert and radiolarite in a total of 13 g
Publikováno v:
Zephyrus, Vol 44, Iss 0 (2009)
RESUMEN: En este trabajo se estudian, a través de técnicas estadísticas multivariantes una serie de raspadores procedentes de la Cueva de la Cantera (León) mediante seis variables morfométricas orientadas a una mejor identificación del «concep
Externí odkaz:
https://doaj.org/article/a5b51effbb324d4e9095a8afc590b984
Autor:
Ana Neira Campos, F. Mallo Fernández
Publikováno v:
Trabajos de Prehistoria, Vol 47, Pp 321-338 (1990)
En este artículo estudiamos tres grupos de materiales líticos procedentes del yacimiento de la «Cueva de la Cantera» (Alcedo, León) que han sido adscritos, durante muchos años, a tres etapas del Paleolítico Superior: Auriñaciense, Magdalenien
Externí odkaz:
https://doaj.org/article/db48f823eddb4bc3a37c034ebbae42e6
Autor:
Esperanza Fernández-Martínez, Diego Herrero Alonso, Fernando Gómez-Fernández, Eduardo Alonso-Herrero, M. Natividad Fuertes-Prieto, Ana Neira-Campos
Publikováno v:
Journal of Lithic Studies, Vol 3, Iss 2 (2016)
A study of the chert nodules found in the Escalada Formation (Carboniferous, Ponga region, Cantabrian Zone) was carried out as a means to characterise a number of lithic raw materials found in several prehistoric sites of the Cantabrian Mountains (NW
Publikováno v:
Journal of Lithic Studies, Vol 3, Iss 2 (2016)
This work provides the keys to the mineralogical and geochemical characterization of black chert from the Vegamián Fm. This formation crops out throughout the whole of the Cantabrian Zone (of Palaeozoic age), one of the geological zones of the Canta