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.