| Reference Type | Journal (article/letter/editorial) |
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| Title | The crystal structure of wolframite type tungstates at high pressure |
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| Journal | Zeitschrift für Kristallographie - Crystalline Materials |
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| Authors | Macavei, J. | Author |
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| Schulz, H. | Author |
| Year | 1993 (January 1) | Volume | 207 |
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| Issue | part-2 |
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| Publisher | Walter de Gruyter GmbH |
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| Download URL | https://rruff.info/doclib/zk/vol207/ZK207_193.pdf+ |
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| DOI | doi:10.1524/zkri.1993.207.part-2.193Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 113899 | Long-form Identifier | mindat:1:5:113899:7 |
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| GUID | 0 |
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| Full Reference | Macavei, J., Schulz, H. (1993) The crystal structure of wolframite type tungstates at high pressure. Zeitschrift für Kristallographie - Crystalline Materials, 207 (part-2) 193 doi:10.1524/zkri.1993.207.part-2.193 |
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| Plain Text | Macavei, J., Schulz, H. (1993) The crystal structure of wolframite type tungstates at high pressure. Zeitschrift für Kristallographie - Crystalline Materials, 207 (part-2) 193 doi:10.1524/zkri.1993.207.part-2.193 |
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| In | (1993, January) Zeitschrift für Kristallographie - Crystalline Materials Vol. 207 (part-2) Walter de Gruyter GmbH |
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| Abstract/Notes | AbstractSingle-crystal structure determinations of wolframite-type structures were performed using a diamond anvil cell with beryllium gaskets. Unit cell parameters of MgWOAll investigated compounds compress anisotropically with theIn all compounds, the WOWith increasing pressure the oxygen atomic positions remain constant within one standard deviation, while the heavy atoms positions show a different pressure dependence: a shift ofWith increasing pressure the A and W cations approach each other, indicating a tendency of a transition from the wolframite structure to the scheelite structure, where the A and W cations lie in the same plane. |
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