Difference between revisions of "Template:Geologic time scale"

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imported>Necessary Evil
(Partial undid revision 445221977 by J4lambert (talk) Something went wrong at the Quaternary section.)
(fixed a typo "Earth's atmosphere become oxygenic" -> "Earth's atmosphere becomes oxygenic)
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|style="background:#b3b25e"| [[Orosirian]]
 
|style="background:#b3b25e"| [[Orosirian]]
|colspan="3"| The [[Earth's atmosphere|atmosphere]] become [[oxygen]]ic. [[Vredefort crater|Vredefort]] and [[Sudbury Basin]] asteroid impacts. Much [[orogeny]]. [[Penokean orogeny|Penokean]] and [[Trans-Hudsonian Orogeny|Trans-Hudsonian Orogenies]] in North America. Early Ruker Orogeny in Antarctica, 2000 - 1700 [[Year#SI_prefix_multipliers|Ma]]. Glenburgh Orogeny, [[Gascoyne Complex|Glenburgh Terrane]], [[Australia (Continent)|Australian Continent]] [[circa|c.]] 2005–1920 [[Year#SI prefix multipliers|Ma]]. Kimban Orogeny, [[Gawler craton]] in Australian Continent begins.
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|colspan="3"| The [[Earth's atmosphere|atmosphere]] becomes [[oxygen]]ic. [[Vredefort crater|Vredefort]] and [[Sudbury Basin]] asteroid impacts. Much [[orogeny]]. [[Penokean orogeny|Penokean]] and [[Trans-Hudsonian Orogeny|Trans-Hudsonian Orogenies]] in North America. Early Ruker Orogeny in Antarctica, 2000 - 1700 [[Year#SI_prefix_multipliers|Ma]]. Glenburgh Orogeny, [[Gascoyne Complex|Glenburgh Terrane]], [[Australia (Continent)|Australian Continent]] [[circa|c.]] 2005–1920 [[Year#SI prefix multipliers|Ma]]. Kimban Orogeny, [[Gawler craton]] in Australian Continent begins.
 
|style="background:#b3b25e"| 2050<ref name="absolute-age" />
 
|style="background:#b3b25e"| 2050<ref name="absolute-age" />
 
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Revision as of 16:23, 26 September 2011