TY - JOUR
T1 - Crystal-chemistry by X-ray structure refinement and electron microprobe analysis of a series of sodic-calcic to alkali- amphiboles from the Nybo eclogite pod, Norway.
AU - Ungaretti, L.
AU - Smith, D. C.
AU - Rossi, G.
PY - 1981
Y1 - 1981
N2 - The crystal structures of 21 amphibole crystals from a single 16 cm-thick layered sample from the Nybo pod, Nordfjord, W Norway, have been refined. Most compositions lie between winchite and the two end-members which are the most substituted Fe-free amphiboles: NaNa2Mg3Al2Si7AlO22(OH)2 here termed nyboite and NaCaNaMg3Al2Si6Al2O22(OH)2, magnesio-alumino-taramite. The main compositional relationships can be explained by a combination of local bulk chemical control, P-T conditions, and site occupancies, thus enabling approximate site occupancy determinations from cell dimensions alone. It is claimed that chemical analyses by XRD structure refinement without chemical restraints are comparable in accuracy to electron microprobe analyses of the same crystals. -R.A.H.
AB - The crystal structures of 21 amphibole crystals from a single 16 cm-thick layered sample from the Nybo pod, Nordfjord, W Norway, have been refined. Most compositions lie between winchite and the two end-members which are the most substituted Fe-free amphiboles: NaNa2Mg3Al2Si7AlO22(OH)2 here termed nyboite and NaCaNaMg3Al2Si6Al2O22(OH)2, magnesio-alumino-taramite. The main compositional relationships can be explained by a combination of local bulk chemical control, P-T conditions, and site occupancies, thus enabling approximate site occupancy determinations from cell dimensions alone. It is claimed that chemical analyses by XRD structure refinement without chemical restraints are comparable in accuracy to electron microprobe analyses of the same crystals. -R.A.H.
UR - http://www.scopus.com/inward/record.url?scp=0019687049&partnerID=8YFLogxK
U2 - 10.3406/bulmi.1981.7486
DO - 10.3406/bulmi.1981.7486
M3 - Article
AN - SCOPUS:0019687049
VL - 104
SP - 400
EP - 412
JO - Bulletin de Mineralogie
JF - Bulletin de Mineralogie
IS - 4
ER -