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Crystal structure refinements of magnesite, calcite, rhodochrosite, siderite, smithonite, and dolomite, with discussion of some aspects of the stereochemistry of calcite type carbonates

·1981·Zeitschrift für Kristallographie - Crystalline Materials

Abstract

The crystal structures of magnesite, calcite, rhodochrosite, siderite, smithonite and dolomite were refined by standard single crystal X-ray methods using diffraction data up to sin[unk]/λ = 1.0 Å−1. The C – O bond lengths are essentially the same. Attention is drawn to short O – O contacts (2.85 Å in both magnesite and smithonite) outside the coordination figures. The MeO 6 octahedra are always elongated parallel [00.1]; the distortion is not a monotone function of the Me – O distance. The approximation of four point charges for the [CO 3]2− ion for calcite gives good agreement between observation and classical electrostatic calculation when charges of 1 + for carbon and 1 − for oxygen are used.

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Research works printed but not linked: 26

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Metadata

Venue
Zeitschrift für Kristallographie - Crystalline Materials
Published
1981-02-01
Volume
156
Issue
3-4
Pages
233-243
ISSN
  • 2194-4946 (ISSN-L)
  • 2196-7105
OpenAlex
W2068000204
Cited by
338
References
0
FWCI
3.13
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Crystal structure refinements of magnesite, calcite, rhodochrosite, siderite, smithonite, and dolomite, with discussion of some aspects of the stereochemistry of calcite type carbonates. https://app.cochat.ai/papers/10.1524/zkri.1981.156.3-4.233
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Crystal structure refinements of magnesite, calcite, rhodochrosite, siderite, smithonite, and dolomite, with discussion of some aspects of the stereochemistry of calcite type carbonates. (1981). Zeitschrift für Kristallographie - Crystalline Materials. https://doi.org/10.1524/zkri.1981.156.3-4.233

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