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  • The crystal structure of troilite from chondrites Etter and Georgetown and a troilite analog synthesized by sulfurization of an iron wire was refined using single-crystal X-ray data. Troilite is known to be hexagonal, with space group P-62c, which is non-centrosymmetric, allowing two non-identical inversely related spatial arrangements of atoms within the unit cell. All three samples represent the so-called inversion twins. They contain both inversely related atomic orientations instead of a single atomic arrangement. The inversion twinning may have developed as a result of a phase transition from the ideal centrosymmetric NiAs-type structure to troilite-type structure during cooling. In addition, all samples were found to be cation-deficient. The departure from ideal stoichiometry-up to almost 3.5 rel% of metal atoms are missing-is also possibly related to atomic ordering when the crystals cooled.
  • The crystal structure of troilite from chondrites Etter and Georgetown and a troilite analog synthesized by sulfurization of an iron wire was refined using single-crystal X-ray data. Troilite is known to be hexagonal, with space group P-62c, which is non-centrosymmetric, allowing two non-identical inversely related spatial arrangements of atoms within the unit cell. All three samples represent the so-called inversion twins. They contain both inversely related atomic orientations instead of a single atomic arrangement. The inversion twinning may have developed as a result of a phase transition from the ideal centrosymmetric NiAs-type structure to troilite-type structure during cooling. In addition, all samples were found to be cation-deficient. The departure from ideal stoichiometry-up to almost 3.5 rel% of metal atoms are missing-is also possibly related to atomic ordering when the crystals cooled. (en)
  • Z monokrystalových rtg. difrakčních dat byly zpřesněny krystalové struktury troilitů z chondritů Etter a Georgetown a analogu troilitu syntetizovaného sulfurizací železného drátu. Všechny vzorky představují tzv. inverzní dvojčata. Dvojčatění vzniklo v důsledku fázového přechodu z ideální centrosymetrické struktury typu NiAs během chladnutí. Navíc všechny vzorky vykazují deficit kovových atomů až do 3.5 rel%. (cs)
Title
  • Inversion twinning in troilite
  • Inversion twinning in troilite (en)
  • Inverzní dvojčatění v troilitu (cs)
skos:prefLabel
  • Inversion twinning in troilite
  • Inversion twinning in troilite (en)
  • Inverzní dvojčatění v troilitu (cs)
skos:notation
  • RIV/67985831:_____/06:00051347!RIV07-GA0-67985831
http://linked.open.../vavai/riv/strany
  • 917;921
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA203/99/M037), P(GA205/02/1101), P(GA205/05/0459), Z(AV0Z30130516)
http://linked.open...iv/cisloPeriodika
  • 5-6
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 480324
http://linked.open...ai/riv/idVysledku
  • RIV/67985831:_____/06:00051347
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • troilite; absolute structure; crystallography; iron monosulfide; iron meteorites (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • US - Spojené státy americké
http://linked.open...ontrolniKodProRIV
  • [E89FD2AEA6C9]
http://linked.open...i/riv/nazevZdroje
  • American Mineralogist
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 91
http://linked.open...iv/tvurceVysledku
  • Skála, Roman
  • Drábek, M.
  • Cisařová, I.
http://linked.open...n/vavai/riv/zamer
issn
  • 0003-004X
number of pages
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