Mineral diversity increased after the Great Oxygenation event.
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Q1: Most basement rock formed during the Archean
Q2: Continental red beds formed before banded iron
Q3: During the Grenville orogeny, an ocean basin
Q5: The Pacific Ocean is in the later
Q6: The Grenville orogeny was the culminating event
Q7: Sandstone-carbonate-shale assemblages are characteristic of the early
Q8: The evolution of Laurentia can be described
Q9: Banded iron formations precipitated in oxygen-rich ocean
Q10: Fortunately for life, oxygen levels in the
Q11: Glaciers were rare during the Proterozoic, as
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