The Ti4+/Ti3+ ratio of magmatic melts: Application to the problem of the reduction of lunar basalts View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2012-07

AUTHORS

A. A. Borisov

ABSTRACT

Using published experimental data an expression was derived for the Ti4+/Ti3+ ratio as a function of temperature, oxygen fugacity, and melt composition. The equation can be used to estimate Ti3+ content in lunar basaltic melts. It was shown that the Ti3+ content in melts is probably no higher than the Fe3+ content even under the reduced conditions typical of lunar magmas. Trivalent Ti can lead to some decrease in during melt cooling under closed-system conditions, but it cannot reduce Fe2+ in melt to metal, because it will be completely consumed by Fe3+ reduction to Fe2+. The presence of additional reducers, such as Cr2+, can be favorable for the formation of metal during melt cooling. More... »

PAGES

391-398

Journal

TITLE

Petrology

ISSUE

4

VOLUME

20

Author Affiliations

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s0869591112040030

DOI

http://dx.doi.org/10.1134/s0869591112040030

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1035684407


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