Artículo
An association of secondary Al-Li-Be-Ca-Sr phosphates in the San Elías pegmatite, San Luis, Argentina
Fecha de publicación:
08/2012
Editorial:
Mineralogical Association of Canada
Revista:
Canadian Mineralogist
ISSN:
0008-4476
Idioma:
Inglés
Tipo de recurso:
Artículo publicado
Clasificación temática:
Resumen
The complex association of secondary phosphates from the Li-bearing, rare-element San Elías pegmatite in the Eastern Pampean ranges of Argentina shows widespread albite-hosted dendritic montebrasite in its northern part and lepidolite in the south. This dendritic montebrasite survived low-temperature processes virtually intact, but subrectangular blocks of montebrasite along the margins of quartz core were extensively modified in three stages: (i) two generations of secondary montebrasite intimately intergrown with hydroxylherderite, augelite, and fluorapatite, (acid hydrous fluids, locally channeled, at ∼450°-420°C, ∼2 kbar); (ii) goyazite-crandallite and hydroxylapatite formed after P-T equilibration between the pegmatite and its host rock along the path of metamorphic cooling, which introduced Ca, Sr and minor S from the host rocks into the pegmatite (at about <300°C); (iii) at a still lower T, the remainder of the primary montebrasite and all of its alteration products were subject to extensive leaching, removal and dispersal of phosphorus, and introduction of Si, generating pseudomorphs consisting mainly of kaolinite, quartz and minor lithian muscovite, K-feldspar (adularia), and traces of residual microlite as remnants of previous alteration stages.
Archivos asociados
Licencia
Identificadores
Colecciones
Articulos(IANIGLA)
Articulos de INST. ARG. DE NIVOLOGIA, GLACIOLOGIA Y CS. AMBIENT
Articulos de INST. ARG. DE NIVOLOGIA, GLACIOLOGIA Y CS. AMBIENT
Citación
Galliski, Miguel Angel; Černý, Petr; Marquez Zavalia, Maria Florencia; Chapman, Ron; An association of secondary Al-Li-Be-Ca-Sr phosphates in the San Elías pegmatite, San Luis, Argentina; Mineralogical Association of Canada; Canadian Mineralogist; 50; 4; 8-2012; 933-942
Compartir
Altmétricas