Melting relationships of Ni-Mg olivines and some geochemical implications

Details Melting relationships of Ni-Mg olivines and some geochemical implications Melting relationships of Ni-Mg olivines and some geochemical implications

Nov 1956

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1956gecoa..10..297r&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 10, Issue 5-6, pp.297-303

Computer Science

5

Scientific paper

A complete series of solid solutions exists in the range Ni 2 SiO 4 -Mg 2 SiO 4 . Temperatures of beginning of melting increase with increasing content of Mg 2 SiO 4 . Solid solutions in the range N 100 -N 50 M 50 melt incongruently with the separation of NiO. In this range, ternary relations obtain. In the range N 50 M 50 -M 100 the system is binary. The behaviour of nickel in magmas is discussed in terms of the experimental data obtained, and it is concluded that nickel enters common olivine at the expense of iron rather than magnesium.

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