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001 | 9.840139 |
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003 | CaOODSP |
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005 | 20221107151753 |
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007 | cr ||||||||||| |
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008 | 170721s1966 oncad ob f000 0 eng d |
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040 | |aCaOODSP|beng |
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043 | |an-cn--- |
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086 | 1 |aM38-8/13E-PDF|zM38-8/13 |
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100 | 1 |aTurnock, Allan C. |
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245 | 10|aSynthetic wodginite, tapiolite and tantalite |h[electronic resource] / |cA.C. Turnock. |
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260 | |aOttawa : |bQueen's Printer, |c1966. |
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300 | |ap. 461-470 : |bcharts, ill. |
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490 | 1 |aReprint series ; |vRS 13 |
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500 | |aCover title. |
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500 | |a"Reprinted from the Canadian Mineralogist, Vol. 8, Part 4, 1966, Pages 461 to 470." |
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500 | |aHistorical publication digitized from print 2017 [by Natural Resources Canada]. |
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504 | |aIncludes bibliographical references. |
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520 | 3 |a"Solid phases in the systems MnTa2O6-FeTa2O6-O and MnTa2O6-FeTaO4 have been synthesized at various temperatures and partial pressures of oxygen. In the binary system MnTa2O6-FeTa2O6, the two solid phases produced were: (i) orthorhombic tantalite, and (ii) tetragonal (tapiolite). The maximum amounts of substitution al 1200 °C were x = 0.18, y = 0.62. The oxidation of these tantalites and tapiolites produced solid phases with compositions that are on the join MnTa2O6-FeTaO4, plus exsolved Ta2O5. In the system MnTa2O6-FeTaO4, the three solid phases produced were: (i) orthorhombic tantalite, (ii) monoclinic wodginite, and (iii) a tetragonal compound with a rutile-type structure. It has been shown that in wodginite (i) the iron is trivalent and the manganese divalent, and that (ii) tin is not an essential component"--Abstract, p. 461. |
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692 | 07|2gccst|aMinerals |
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710 | 1 |aCanada. |bNatural Resources Canada. |
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710 | 1 |aCanada. |bDepartment of Energy, Mines and Resources. |
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710 | 1 |aCanada. |bMines Branch. |
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830 | #0|aReprint series - Dept. of Energy, Mines and Resources, Mines Branch ;|vRS 13|w(CaOODSP)9.834843 |
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856 | 40|qPDF|s4.81 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M38-8/M38-8-13-eng.pdf |
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