10 March 2023 1 8K Report

Hello everyone,

I would like to know that does re-heating modify the composition of a olivine-hosted melt inclusion in basaltic rocks? For example, unheated olivine-hosted MIs show the SiO2 value ~69 wt%. However, heated MIs show the same composition as basaltic rocks(SiO2=50 wt%)

The heated MIs and unheated MIs are not the same olivine-hosted grains, but the same one basaltic rocks sample.

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