Zobrazeno 1 - 10
of 15
pro vyhledávání: '"T. S. Ercit"'
Autor:
T. S. Ercit
Publikováno v:
Mineralogical Magazine. 74:715-730
The crystal chemistry of tapiolite is more complicated than previously recognized. Perusal and synthesis of relatively recent publications reveals a ‘hidden’ story about tapiolite, one that: (1) permits quantification of the effects of Mn, Fe3+,
Publikováno v:
Mineralogical Magazine. 73:1033-1050
Holtite, approximately (Al,Ta,□)Al6(BO3)(Si,Sb3+,As3+)Σ3O12(O,OH,□s)Σ3, is a member of the dumortierite group that has been found in pegmatite, or alluvial deposits derived from pegmatite, at three localities: Greenbushes, Western Australia; Vo
Publikováno v:
American Mineralogist. 93:702-706
Publikováno v:
American Mineralogist. 93:252-256
Publikováno v:
American Mineralogist. 92:703-707
Autor:
T. S. Ercit
Publikováno v:
American Mineralogist. 91:1201-1209
Publikováno v:
Mineralogy and Petrology. 54:93-103
Summary Nodular anorthosite, containing rounded aggregates (nodules) of plagioclase set in a gabbroic to pyroxenitic matrix, is developed in constrictions ( < 500 m wide) within the central and eastern parts of the Early Proterozoic East Bull Lake In
Publikováno v:
Mineralogy and Petrology. 48:235-255
The crystal structure of cesstibtantite has been solved from diffractometer data collected on samples from Leshaia, Russia and the Tanco pegmatite, Manitoba. Cesstibtantite from the Leshaia pegmatite (type locality) hasa 10.515(2) A, space groupFd3m,
Refinement of the structure of ?-Nb2O5 and its relationship to the rutile and thoreaulite structures
Autor:
T. S. Ercit
Publikováno v:
Mineralogy and Petrology. 43:217-223
The crystal structure of ζ-Nb2O5, space groupC2/c, a 12.740(2),b 4.8830(6),c 5.5609(6)A,β 105.02(1)°, Z 4, has been refined toR 1.6% for 457 observed reflections (MoKα). The coordination polyhedron of the niobium atom is a distorted octahedron; t
Publikováno v:
The Canadian Mineralogist. 38:765-766
[Galuskin & Galuskina (2000)][1] seem unaware of the requirements for defining and naming a new mineral species. These requirements are set out in detail by the Commission on New Minerals and Mineral Names of the International Mineralogical Associati