释义 |
reedmergnerite Min.|riːdˈmɜːgnəraɪt| [See quot. 1954 and -ite1.] A colourless triclinic silicate of sodium and boron, NaBSi3O8.
1954C. Milton et al. in Bull. Geol. Soc. Amer. LXV. 1286 Cores and cuttings from the Green River formation in Utah contain two new minerals, reedmergnerite and eitelite,..in dolomitic shale. Reedmergnerite..occurs in many wells in Duchesne and Uintah counties as crystals rarely more than 1 mm long, colorless, triclinic..; habit stubby prismatic... The name honors Frank S. Reed and John L. Mergner, technicians of the Geological Survey. 1974Amer. Mineralogist LIX. 79/1 This study was undertaken to determine more precisely the bond lengths and angles of danburite..for comparison with topologically similar paracelsian (BaAl2Si2O8) and hurlbutite (CaBe2P2O8) and with structurally similar feldspars: anorthite (CaAl2Si2O8)..; albite (NaAlSi3O8); and reedmergnerite (NaBSi3O8). |