quartz,feldspar and halite,are they good candidates for isolating hazard materials?and why?
Many diamonds have inner lines of olivine trapped interior them for the most area , reckoning on the creation element and the encircling enviorment i'd imagine some thing is accessible.Quartz is continually contemporary in igneous for the most area in really 2 diverse ranges , one immediately from the magma or hydro thermally after cooling.i imagine the reply on your question may be pegmatitic.
Because forsterite reacts with quartz to form the orthopyroxene mineral enstatite in the following reaction: Mg2SiO4 + SiO2 → 2 MgSiO3.
