Definition of magnesiochromite in English:

magnesiochromite

noun maɡˌniːzɪəʊˈkrəʊmʌɪt

Mineralogy

Originally: a mineral, (Mg,Fe)Cr₂O₄, analogous to chromite (FeCr₂O₄), with magnesium replacing much of the iron. Now usually: a spinel of the general formula (Mg,Fe)(Cr,Al)₂O₄, specifically the endmember, MgCr₂O₄ (picrochromite).

Origin

Late 19th century; earliest use found in Edward Dana (1849–1935), mineralogist and physicist. From magnesium + -o- + chromite; introduced as a more transparent substitute for German Magnochromit, after earlier magnesioferrite.

Definition of magnesiochromite in US English:

magnesiochromite

nounmaɡˌniːzɪəʊˈkrəʊmʌɪt

Mineralogy

Originally: a mineral, (Mg,Fe)Cr₂O₄, analogous to chromite (FeCr₂O₄), with magnesium replacing much of the iron. Now usually: a spinel of the general formula (Mg,Fe)(Cr,Al)₂O₄, specifically the endmember, MgCr₂O₄ (picrochromite).

Origin

Late 19th century; earliest use found in Edward Dana (1849–1935), mineralogist and physicist. From magnesium + -o- + chromite; introduced as a more transparent substitute for German Magnochromit, after earlier magnesioferrite.

单词	magnesiochromite
释义	Definition of magnesiochromite in English: magnesiochromite noun maɡˌniːzɪəʊˈkrəʊmʌɪt Mineralogy Originally: a mineral, (Mg,Fe)Cr₂O₄, analogous to chromite (FeCr₂O₄), with magnesium replacing much of the iron. Now usually: a spinel of the general formula (Mg,Fe)(Cr,Al)₂O₄, specifically the endmember, MgCr₂O₄ (picrochromite). Origin Late 19th century; earliest use found in Edward Dana (1849–1935), mineralogist and physicist. From magnesium + -o- + chromite; introduced as a more transparent substitute for German Magnochromit, after earlier magnesioferrite. Definition of magnesiochromite in US English: magnesiochromite nounmaɡˌniːzɪəʊˈkrəʊmʌɪt Mineralogy Originally: a mineral, (Mg,Fe)Cr₂O₄, analogous to chromite (FeCr₂O₄), with magnesium replacing much of the iron. Now usually: a spinel of the general formula (Mg,Fe)(Cr,Al)₂O₄, specifically the endmember, MgCr₂O₄ (picrochromite). Origin Late 19th century; earliest use found in Edward Dana (1849–1935), mineralogist and physicist. From magnesium + -o- + chromite; introduced as a more transparent substitute for German Magnochromit, after earlier magnesioferrite.
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