Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Rafael Pablo Lozano Fernández"'
Autor:
José Manuel Compaña Prieto, Kelvin dos Santos Alves, Raúl Merinero Palomares, Santos Barrios Sánchez, Juan Gómez Barreiro, Rafael Pablo Lozano Fernández
In this contribution we have investigated the Fresnedoso Quaternary gold placer (Western Spain), analyzing the morphotextural and microchemical evolution of gold particles. The statistical analysis has revealed the presence of two populations of part
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b011e32afe2ef474799db049e4996d8e
https://doi.org/10.5194/egusphere-egu21-12077
https://doi.org/10.5194/egusphere-egu21-12077
Autor:
Juan Gómez Barreiro, Mercedes Suárez Barrios, Jeremi Malecki, Raúl Merinero Palomares, Santos Barrios, Juan Morales Sánchez-Migallón, Rafael Pablo Lozano Fernández, Kelvin dos Santos Alves
Gold placers are abundant and intensively surveyed in western Iberia since antiquity. Three Cenozoic gold placers covering Neoproterozoic-Lower Paleozoic basement rocks have recently been revealed, which stand out for the number and size of the sampl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a59eb60f245a0dcaca11729360d32d1e
https://doi.org/10.5194/egusphere-egu21-13358
https://doi.org/10.5194/egusphere-egu21-13358
Publikováno v:
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Andean geology v.45 n.2 2018
SciELO Chile
CONICYT Chile
instacron:CONICYT
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Andean geology v.45 n.2 2018
SciELO Chile
CONICYT Chile
instacron:CONICYT
The A-type Huaco granite pluton of the Velasco range (Sierras Pampeanas of northwest Argentina) is formed by three coeval granitic facies and contains subordinate coeval-to-late facies, as well as enclaves, dikes and stocks that show different tempor
Publikováno v:
European Journal of Mineralogy. 21:783-794
The fulgurite of Torre de Moncorvo (Portugal) was formed by lightning striking a small electricity pylon; it consists morphologically of a central cylinder with radial ramifications several metres long. It is largely composed of glass, with the remai