| 释义 |
magnesioriebeckite, n. Min.
Brit. |magˌniːziəʊˈriːbəkʌɪt|, |magˌniːziəʊˈriːbɛkʌɪt|, U.S. |mægˌnizioʊˈribəˌkɑɪt|, |mægˌnizioʊˈribɛkˌɑɪt|
[‹ magnesium n. + -o- connective + riebeckite n.]
A riebeckite in which the amount of magnesium is equal to or greater than that of iron(ii).
1957A. Miyashiro in Jrnl. Faculty Sci. Tokyo Univ. Section II 11 63 Their magnesium analogues will be called magnesioriebeckite. 1992W. A. Deer et al. Introd. Rock-forming Minerals (ed. 2) 262 Alkali amphiboles..with ‹0.5(Na+K) in A are members of a solid-solution series defined by four end-members, glaucophane, magnesioriebeckite, ferroglaucophane and riebeckite. |