Zobrazeno 1 - 8
of 8
pro vyhledávání: '"granitic facies"'
Publikováno v:
Journal of Maps, Vol 13, Iss 2, Pp 684-697 (2017)
The Valle Mosso pluton (VMP) is a Permian granitic body intruded at intermediate to upper crustal levels in the rocks of the pre-Alpine basement of the Ivrea-Verbano Zone and Serie dei Laghi shortly after the end of Variscan orogeny. As a consequence
Externí odkaz:
https://doaj.org/article/6d8a1bce34dc42749a865fce9205196d
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:
Journal of Maps, Vol 13, Iss 2, Pp 684-697 (2017)
The Valle Mosso pluton (VMP) is a Permian granitic body intruded at intermediate to upper crustal levels in the rocks of the pre-Alpine basement of the Ivrea-Verbano Zone and Serie dei Laghi shortly after the end of Variscan orogeny. As a consequence
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5556a853834dde8a2409824416a24468
Publikováno v:
Repositório Institucional da UNESPUniversidade Estadual PaulistaUNESP.
Submitted by PEDRO LUIZ LUPPI FOSTER null (luppifoster@gmail.com) on 2016-11-16T19:23:57Z No. of bitstreams: 1 Tese_Mestrado_Pedro_Foster.pdf: 23543008 bytes, checksum: 970cd8b58cfa88e2188ef3b76510d096 (MD5)
Approved for entry into archive by Fe
Approved for entry into archive by Fe
Externí odkaz:
http://hdl.handle.net/11449/144675
Publikováno v:
Repositório Institucional da UNESP
Universidade Estadual Paulista (UNESP)
instacron:UNESP
Universidade Estadual Paulista (UNESP)
instacron:UNESP
Submitted by PEDRO LUIZ LUPPI FOSTER null (luppifoster@gmail.com) on 2016-11-16T19:23:57Z No. of bitstreams: 1 Tese_Mestrado_Pedro_Foster.pdf: 23543008 bytes, checksum: 970cd8b58cfa88e2188ef3b76510d096 (MD5) Approved for entry into archive by Felipe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3056::ba9b85c9aa3b9c05815b347ea7a3ce17
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5793dbb9860ff6d000d1ac5b34f401ff
https://doi.org/10.5027/andgeov45n2-3015
https://doi.org/10.5027/andgeov45n2-3015
Akademický článek
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Akademický článek
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