INGEIS   05370
INSTITUTO DE GEOCRONOLOGIA Y GEOLOGIA ISOTOPICA
Unidad Ejecutora - UE
congresos y reuniones científicas
Título:
PAULINGITE FROM JUNIN DE LOS ANDES, PATAGONIA, ARGENTINA
Autor/es:
MARIA ELENA VATTUONE; SABRINA CROSTA; LATORRE, CARLOS OSCAR; LEAL, PABLO; BERBEGLIA, YANINA
Lugar:
Santa Fe, EEUU
Reunión:
Congreso; 44° Annual Meeting of the Clay Mineral Society; 2007
Resumen:
Paulingite in assemblage with Ca-K-Na
phillipsite and chabazite was found on the border of amygdales of Tertiary
amygdaloid alkaline basalts located near Junin de los Andes, Patagonia. The outcrop is located at 39°54'57" south
and 71°03'10" west. The zeolites were studied by SEM, EDS and XRD.
Analcime, natrolite, thomsonite, mesolite and
scolecite also occurs filing different amygdales. In the matrix of
these rocks, there are albite, interestratified chlorite/smectite, pumpellyite,
and very scarce yugawaralite. Altered olivine and fresh pyroxene are the
primary minerals that remain in few samples of these rocks (Vattuone et al.,
2006).
Paulingite is isotropic
with dodecahedral, trapezohedral and cubic forms (Fig. 1). The XRD spacings
are coincident with 39-1378 JCPDS-ICDD (1994). The parameters of the unit cell
are: a0 = 35.10 Å, according to Armbruster and Gunter (2001). Table
1 shows a chemical composition that evidences a low Tsi= 0.71/0.72. The amount
of Ca and K indicate that this paulingite is in the range proposed by Passaglia
and Sheppard (2001) for this species. The paulingite-phillipsite assemblage
indicates that temperature of formation occurs in 60°C/80°C range (Deer et al., 2004). On the other hand their
crystallization in basalt amygdales suggests deuteric processes.