Thalénite-(Y) from Golden Horn Batholith, Washington State

database, nuove specie, discrediti,
ridefinizioni, classificazioni, ecc.
Rispondi
Avatar utente
Marco E. Ciriotti
Messaggi: 23422
Iscritto il: ven 25 giu, 2004 11:31
Località: via San Pietro, 55 I-10073 Devesi/Cirié TO - Italy
Contatta:

Thalénite-(Y) from Golden Horn Batholith, Washington State

Messaggio da Marco E. Ciriotti » mar 11 lug, 2017 11:53

Prossima pubblicazione.

Referenza:
▪ Raschke, M.B., Anderson, E.J.D., Van Fosson, J., Allaz, J., Smyth, J.R., Škoda, R., Persson, P.M., Becker, R. (2017): Thalénite-(Y) from Golden Horn Batholith, Washington State, and comparison with new analyses from the White Cloud Pegmatite, Pikes Peak Batholith, Colorado, USA. Mineralogical Magazine, 81, (in press).

Abstract:
Thalénite-(Y) (ideally Y3Si3O10F) is a heavy-rare-earth-rich silicate phase occurring in granite pegmatites that may help to illustrate REE chemistry and behavior in natural systems. Crystal structure and mineral chemistry of thalénite-(Y) was analyzed by electron microprobe analysis, X-ray diffraction, and micro-Raman spectroscopy comparing thalénite-(Y) from a new locality in the peralkaline granite of the Golden Horn Batholith, Okanogan County, Washington State, USA, in comparison with new analyses of thalénite-(Y) from the White Cloud pegmatite in the Pikes Peak batholith, Colorado, USA. The Golden Horn thalénite-(Y) occurs as late stage sub-millimeter euhedral bladed transparent crystals in small miarolitic cavities in an arfvedsonite-bearing biotite granite. It exhibits growth zoning with distinct HREE vs. LREE-enriched zones. The White Cloud thalénite-(Y) occurs in two distinct anhedral and botryoidal crystal habits of mostly homogenous composition. In addition, minor secondary thalénite-(Y) is recognized by its distinct Yb-rich composition (up to 0.8 apfu Yb). Single-crystal X-ray diffraction analysis and structure refinement reveals Y-site ordering with preferential HREE occupation of Y2 vs. Y1 and Y3 REE sites. Chondrite normalization shows continuous enrichment of HREE in White Cloud thalénite-(Y), in contrast to Golden Horn thalénite-(Y) with a slight depletion of the heaviest REE (Tm, Yb and Lu). The results suggest a hydrothermal origin of the Golden Horn miarolitic thalénite-(Y), compared to a combination of both primary magmatic followed by hydrothermal processes responsible for the multiple generations and a range of spatial scales in White Cloud thalénite-(Y).
Marco E. Ciriotti

«Things are interesting only in so far as they relate themselves to other things»

Rispondi

Chi c’è in linea

Visitano il forum: Nessuno e 3 ospiti