koechliniten.

/ˈkəːxlᵻnʌɪt/

/ˈkəːklᵻnʌɪt/

Etymology: < the name of Rudolf Koechlin (1862–1939), curator of the mineral collection, Hof-Museum, Vienna + -ite suffix¹.

Mineralogy.

A molybdate of bismuth, Bi₂MoO₆, found as minute, greenish-yellow plates, and in soft white to yellow masses.

ΘΚΠ

the world > the earth > minerals > types of mineral > tungstates and molybdates > [noun] > other molybdates

koechlinite1914

lindgrenite1935

umohoite1953

1914 W. T. Schaller in Jrnl. Washington Acad. Sci. IV. 354 Koechlinite (bismuth molybdate), a new mineral from Schneeberg, Saxony.

1916 W. T. Schaller in Bull. U.S. Geol. Surv. No. 610. 14 Koechlinite is clearly a secondary mineral formed in the cavities of the quartz rock by the reaction of different solutions, one containing bismuth and the other molybdenum.

1943 Amer. Mineralogist 28 537 Koechlinite also was found as soft white to yellow masses associated with bismoclite on specimens from Bygoo, New South Wales. Here, too, the mineral has formed by the alteration of a pre-existing bismuth mineral.

1966 Jrnl. Inorg. & Nuclear Chem. 28 1125 The lattice parameters were equal to those of natural koechlinite within the experimental error.

This entry has not yet been fully updated (first published 1933; most recently modified version published online June 2018).

单词	koechlinite
释义	koechliniten. /ˈkəːxlᵻnʌɪt//ˈkəːklᵻnʌɪt/ Etymology: < the name of Rudolf Koechlin (1862–1939), curator of the mineral collection, Hof-Museum, Vienna + -ite suffix¹. Mineralogy. A molybdate of bismuth, Bi₂MoO₆, found as minute, greenish-yellow plates, and in soft white to yellow masses. ΘΚΠ the world > the earth > minerals > types of mineral > tungstates and molybdates > [noun] > other molybdates koechlinite1914 lindgrenite1935 umohoite1953 1914 W. T. Schaller in Jrnl. Washington Acad. Sci. IV. 354 Koechlinite (bismuth molybdate), a new mineral from Schneeberg, Saxony. 1916 W. T. Schaller in Bull. U.S. Geol. Surv. No. 610. 14 Koechlinite is clearly a secondary mineral formed in the cavities of the quartz rock by the reaction of different solutions, one containing bismuth and the other molybdenum. 1943 Amer. Mineralogist 28 537 Koechlinite also was found as soft white to yellow masses associated with bismoclite on specimens from Bygoo, New South Wales. Here, too, the mineral has formed by the alteration of a pre-existing bismuth mineral. 1966 Jrnl. Inorg. & Nuclear Chem. 28 1125 The lattice parameters were equal to those of natural koechlinite within the experimental error. This entry has not yet been fully updated (first published 1933; most recently modified version published online June 2018). < n.1914
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