Zobrazeno 1 - 10
of 80
pro vyhledávání: '"Sytle M. Antao"'
Autor:
Sytle M. Antao, James W. Nicholls
Publikováno v:
Frontiers in Earth Science, Vol 6 (2018)
Natural nepheline (Nph) samples are intermediate members of solid solutions that extend from the pure Na end-member Na[AlSiO4] to the pure K end-member K[AlSiO4] (=kalsilite, Kls). We examined two volcanic nepheline (ideally, K2Na6[Al8Si8O32] or Nph0
Externí odkaz:
https://doaj.org/article/2956f89b53864a5283230edd14080a84
Autor:
Guy L. Hovis, Sytle M. Antao
Publikováno v:
American Mineralogist. 106:801-811
The crystal structures of 19 samples from the nepheline (NaAlSiO4; Ne)–kalsilite (KAlSiO4; Ks) series, previously prepared via ion-exchange, were examined using synchrotron high-resolution powder X-ray diffraction (HRPXRD) data and Rietveld structu
Autor:
Darren A. Umbsaar, Sytle M. Antao
Publikováno v:
Minerals; Volume 12; Issue 1; Pages: 42
Minerals, Vol 12, Iss 42, p 42 (2022)
Minerals, Vol 12, Iss 42, p 42 (2022)
The crystal structure of four samples from natural wolframite solid solutions, (Fe,Mn)WO4, was obtained with synchrotron high-resolution powder X-ray diffraction (HRPXRD) data, Rietveld refinements, space group P2/c, and Z = 2. Wolframite solid solut
Autor:
Sytle M. Antao, M. Mashrur Zaman
Publikováno v:
Minerals, Vol 11, Iss 16, p 16 (2021)
Minerals
Volume 11
Issue 1
Minerals
Volume 11
Issue 1
This study examines two pegmatitic monazite samples (2a and 4b, these numbers are related to a previous study) to determine their crystal chemistry and effects of internal radiation damage using synchrotron high-resolution powder X-ray diffraction an
Autor:
Sytle M. Antao
Publikováno v:
Minerals, Vol 11, Iss 1320, p 1320 (2021)
Minerals; Volume 11; Issue 12; Pages: 1320
Minerals; Volume 11; Issue 12; Pages: 1320
The crystal structure of two different samples of pyrope garnet, ideally Mg3Al2Si3O12, from South Africa was refined using the Rietveld method, space group Ia3¯d, and monochromatic synchrotron high-resolution powder X-ray diffraction (HRPXRD) data.
Autor:
Sytle M. Antao
Publikováno v:
Minerals, Vol 11, Iss 325, p 325 (2021)
Minerals
Volume 11
Issue 3
Minerals
Volume 11
Issue 3
Synchrotron high-resolution powder X-ray diffraction (HRPXRD) and Rietveld structure refinements were used to examine the crystal structure of single phases and intergrowths (either two or three phases) in 13 samples of the helvine-group minerals, (Z
Autor:
Sytle M. Antao, M. Mashrur Zaman
Publikováno v:
Minerals, Vol 10, Iss 1028, p 1028 (2020)
Minerals
Volume 10
Issue 11
Minerals
Volume 10
Issue 11
This study investigates the crystal chemistry of monazite (APO4, where A = Lanthanides = Ln, as well as Y, Th, U, Ca, and Pb) based on four samples from different localities using single-crystal X-ray diffraction and electron-probe microanalysis. The
Autor:
Sytle M. Antao, M. Mashrur Zaman
Publikováno v:
Minerals, Vol 10, Iss 947, p 947 (2020)
Minerals
Volume 10
Issue 11
Minerals
Volume 10
Issue 11
This study investigates the variations of structural parameters and chemistry of a partially metamict and seven detrital zircon samples from different localities using single-crystal X-ray diffraction, synchrotron high-resolution powder X-ray diffrac
Autor:
Laura A. Cruickshank, Sytle M. Antao
Publikováno v:
Acta Crystallographica Section B Structural Science, Crystal Engineering and Materials. 74:104-114
Cubic garnet (space group Ia\overline 3 d) has the general formula X 3 Y 2 Z 3O12, where X, Y and Z are cation sites. In the tetragonal garnet (space group I41/acd), the corresponding cation sites are X1 and X2, Y, and Z1 and Z2. In both space groups
Autor:
Sytle M. Antao, Inayat Dhaliwal
Publikováno v:
Journal of Synchrotron Radiation. 25:214-221
The crystal structure of four Pb apatite samples, Pb5(BO4)3Cl, was refined with synchrotron high-resolution powder X-ray diffraction data, Rietveld refinements, space group P63/m and Z = 2. For this isotypic series, B = P5+ is pyromorphite, B = As5+