Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Fernando Guillermo Sardi"'
Publikováno v:
Brazilian Journal of Geology, Vol 51, Iss 3 (2021)
Abstract Two porphyritic granitoids (Huaco and Sanagasta) in the Velasco district of the Pampeana Pegmatite Province in Northwestern Argentina are recognized. They are considered the fertile granites of the beryl-bearing pegmatites and can be describ
Externí odkaz:
https://doaj.org/article/34c5e822752b4e49b5b1d986192ab6c2
Publikováno v:
Andean Geology. 50:150
The Reflejos de Mar Li-pegmatite, located in northwestern Argentina, is part of the Villismán pegmatite group, Ancasti District, Pampean Pegmatite Province. Four garnet crystals from the outermost part of the pegmatite were analyzed by major and min
Autor:
Silvana Elizabeth Marangone, Anja M. Schleicher, Kathleen Marie Griffin, Uwe Altenberger, Fernando Guillermo Sardi, Clara E. Cisterna
Publikováno v:
Journal of South American Earth Sciences
The Villismán pegmatite group belonging to the Ancasti district of the Pampean Pegmatite Province is geologically formed by banded schists of the Ancasti Formation which are intruded by the homonymous granitic stock and Li-pegmatites. It is located
Publikováno v:
The Canadian Mineralogist. 52:809-836
Rare-element class, beryl type, beryl-columbite-phosphate subtype pegmatites of the Velasco district from the Pampeana Pegmatite Province, Argentina, contain varieties of green, yellow, and aquamarine beryl. The major and trace element chemistry and
Publikováno v:
Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 258:61-71
The Carboniferous post-orogenic Huaco and Sanagasta granites are located in the central sector of the Velasco Range, northwestern Argentina, and host rare-element (Be) pegmatites. They are highly fractionated peraluminous granites with porphyritic te
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:
Andean geology, Volume: 43, Issue: 1, Pages: 104-86, Published: JAN 2016
Andean geology v.43 n.1 2016
SciELO Chile
CONICYT Chile
instacron:CONICYT
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Andean geology v.43 n.1 2016
SciELO Chile
CONICYT Chile
instacron:CONICYT
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
The specialized leuco-monzogranite of the La Chinchilla Stock is a small Carboniferous stock located in the center of the Velasco Range, Pampean Province, La Rioja, Argentina. It is highly evolved and locally F- andBe-bearing, and has the potential f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::99c711e4dff42fb1e6c00a26d74cc307
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062016000100005&lng=en&tlng=en
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062016000100005&lng=en&tlng=en
Autor:
Fernando Guillermo Sardi
Publikováno v:
Neues Jahrbuch für Geologie und Paläontologie - Monatshefte. 2005:513-528
The Angulos W-Mo-bearing ore deposit is located in the center-eastern region of the Famatina System, NW Argentina. The W-Mo mineralization in Angulos is genetically associated with the Potrerillos Granite, which is the host rock of the deposit. Re-Os
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aabbcc33ac65e34fd5bd4687e8207a53
https://www.ingentaconnect.com/content/schweiz/njbgeol/2012/00000266/00000002/art00005
https://www.ingentaconnect.com/content/schweiz/njbgeol/2012/00000266/00000002/art00005
Autor:
Fernando Guillermo Sardi
The Velasco Pegmatitic District is located in the Velasco range, La Rioja province, northwestern Argentina. The Velasco range is made up of several granitic units of different petrography, magmatic evolution and age among which are the Huaco and Sana
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::34c9602dd68eeec3c6a0e6e953329711
https://gem-a.com/images/Documents/JoG/JoG2008_31_3-4.pdf
https://gem-a.com/images/Documents/JoG/JoG2008_31_3-4.pdf