Fix coherence errors: IOCG deposits tend to accumulate within iron-rich rocks such as banded iron formations, iron schists, etcetera, although iron enrichment of siliciclastic rocks by metasomatism is also recognised within some areas.
IOCG deposits tend to accumulate within iron-rich rocks such as banded iron formations, iron schists, etcetera. Iron enrichment of siliciclastic rocks by metasomatism is also recognised within some areas.