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  • Fe2+ and Mg distribution on octahedral M1 and M2 sites of the orthopyroxene structure is an indicator of the cooling rate and closure temperature of the mineral. It is generally obtained by single-crystal X-ray diffraction, which is limited in spatial resolution. In this work, we determine the cationic distribution at a submicrometer scale in a transmission electron microscope using precession electron diffraction.
  • Fe2+ and Mg distribution on octahedral M1 and M2 sites of the orthopyroxene structure is an indicator of the cooling rate and closure temperature of the mineral. It is generally obtained by single-crystal X-ray diffraction, which is limited in spatial resolution. In this work, we determine the cationic distribution at a submicrometer scale in a transmission electron microscope using precession electron diffraction. (en)
Title
  • Ordering state in orthopyroxene as determined by precession electron diffraction
  • Ordering state in orthopyroxene as determined by precession electron diffraction (en)
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  • Ordering state in orthopyroxene as determined by precession electron diffraction
  • Ordering state in orthopyroxene as determined by precession electron diffraction (en)
skos:notation
  • RIV/68378271:_____/13:00425080!RIV14-AV0-68378271
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  • I
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  • 8-9
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  • 94569
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  • RIV/68378271:_____/13:00425080
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  • orthopyroxene; precession electron diffraction; structure refinement; transmission electron microscopy (en)
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  • US - Spojené státy americké
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  • [43CE6095A47A]
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  • American Mineralogist
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  • 98
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  • Palatinus, Lukáš
  • Cuvillier, P.
  • Cámara, F.
  • Domeneghetti, C.
  • Jacob, D.
  • Leroux, H.
http://linked.open...ain/vavai/riv/wos
  • 000323584000017
issn
  • 0003-004X
number of pages
http://bibframe.org/vocab/doi
  • 10.2138/am.2013.4296
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