Zobrazeno 1 - 7
of 7
pro vyhledávání: '"VELASCO RANGE"'
Publikováno v:
Andean geology, Volume: 45, Issue: 2, Pages: 229-248, Published: MAY 2018
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______614::62e62b45948ff98121707837ca24e382
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062018000200229&lng=en&tlng=en
http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-71062018000200229&lng=en&tlng=en
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
Akademický článek
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Publikováno v:
Rev. Asoc. Geol. Argent. 2010;67(4):425-438
Biblioteca Digital (UBA-FCEN)
Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
instacron:UBA-FCEN
Biblioteca Digital (UBA-FCEN)
Universidad Nacional de Buenos Aires. Facultad de Ciencias Exactas y Naturales
instacron:UBA-FCEN
Along the eastern front of the Sierra de Velasco and at the southern end of the Sierra de Ambato, western Sierras Pampeanas, have been found new evidences of Quaternary tectonic activity near La Rioja city. Observed evidences correspond to different
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3056::bf96ce83555dff6e5c2216e8c656c538
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
Akademický článek
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