Abstract
The thermal stability of reagent-grade calcite and limestone samples with high and low content of iron compounds was compared. The causes of the revealed differences were discussed.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
