Шаблон:Геолошка временска скала/Неоархаик-обележја
Stabilization of most modern cratons; possible mantle overturn event. Insell Orogeny, 2650 ± 150 MYA. Abitibi greenstone belt in present-day Ontario and Quebec begins to form, stablizes by 2600 MYA.
Stabilization of most modern cratons; possible mantle overturn event. Insell Orogeny, 2650 ± 150 MYA. Abitibi greenstone belt in present-day Ontario and Quebec begins to form, stablizes by 2600 MYA.