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Partition of Mg and Fe2+in coexisting pyroxenes

โœ Scribed by M. E. Fleet

Book ID
104764142
Publisher
Springer
Year
1974
Tongue
English
Weight
367 KB
Volume
44
Category
Article
ISSN
0010-7999

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๐Ÿ“œ SIMILAR VOLUMES

Mg, Fe2+site occupancies in coexisting p
Mg, Fe2+site occupancies in coexisting pyroxenes
โœ M. E. Fleet ๐Ÿ“‚ Article ๐Ÿ“… 1974 ๐Ÿ› Springer ๐ŸŒ English โš– 513 KB

The separate distributions for MgSiOa and FeSiO 3 in coexisting pyroxenes from the Skaergaard and Bushveld intrusions and charnockites, which were introduced in an earlier communication, indicate directly that significant amounts of both Fe 2+ and Mg were present in the M(2) site of the Ca-rich pyro

Partition of major and minor elements an
Partition of major and minor elements and equilibration in coexisting pyroxenes
โœ M. E. Fleet ๐Ÿ“‚ Article ๐Ÿ“… 1974 ๐Ÿ› Springer ๐ŸŒ English โš– 879 KB

The partition of Si, A1, Ti, Fe 3+, Mg, Fe 2+, Mn, Ca and Na between coexisting Carich and Ca-poor pyroxenes from a wide variety of igneous and metamorphic rocks have been investigated systematically. Many of the distributions, and especially those for the partition of Ti, Mg, Fe 2+, Mn and Na, indi

Fe2+-Mg2+partition between coexisting co
Fe2+-Mg2+partition between coexisting cordierite and garnet โ€” a discussion of the experimental data
โœ Bernard J. Wood ๐Ÿ“‚ Article ๐Ÿ“… 1973 ๐Ÿ› Springer ๐ŸŒ English โš– 358 KB

The partition of iron and magnesium between cordierite and garnet depends on P]~o as well as temperature. The apparently conflicting experimental data on the values of K D may be reconciled by considering the P]~O pertaining during the different experiments.