Abstract
About 60 ore objects, including large and giant deposits of banded iron formation and related rich iron ores, are known from the Kursk magnetic anom� aly (KMA). One of the largest deposits is the Stoilo deposit, whose geological structure is shown in Fig. 1. An important component of carbonaceous schists and iron formation, as well as deposits of rich iron ores
Full Text
Sign-in/Register to access full text options
Published version (Free)
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have