Banded iron formation (Q43383): Difference between revisions
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Revision as of 19:43, 5 July 2023
Commonly termed BIFs by geologists, they are iron-rich rocks almost always of Precambrian age, predominantly associated with the great oxygenation event (GOE) about 2
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | Banded iron formation |
Commonly termed BIFs by geologists, they are iron-rich rocks almost always of Precambrian age, predominantly associated with the great oxygenation event (GOE) about 2 |
