Archean age oor Spaans

Archean age

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Love compounds have wafted in spring breezes since the Archean age.
Muévete, la orden se está enfriandoLiterature Literature
So many things happened that is it hard to describe everything in one page, so try the Exploratour on The Archean Age, found at the bottom of this page.
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From 3.5 BYA to 2.5 BYA, or roughly to the end of the Archean age, iron ores began to be formed in large amounts at the bottom of the ocean.
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From 3.5 BYA to 2.5 BYA, or roughly to the end of the Archean age, iron ores began to be deposited in large amounts at the bottom of the ocean.
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In contrast to the deep-water deposits of the Archean, the Proterozoic features many strata that were laid down in extensive, shallow epicontinental seas; furthermore, many of these rocks are less metamorphosed than Archean-age ones, and plenty are in fact unaltered.[13]p315 Study of these rocks show that the eon featured rapid continental accretion (unique to the Proterozoic), supercontinent cycles, and wholly-modern orogenic activity.[13]p315/8; 329/32
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In contrast to the deep-water deposits of the Archean, the Proterozoic features many strata that were laid down in extensive shallow epicontinental seas; furthermore, many of these rocks are less metamorphosed than Archean-age ones, and plenty are unaltered.[4]:315 Study of these rocks shows that the eon continued the massive continental accretion that had begun late in the Archean, as well as featured the first definitive supercontinent cycles and wholly modern orogenic activity.[4]:315–18, 329–32
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The Archean The Archean is the name of the age which began with the forming Earth.
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The Archean is the name of the age which began with the forming Earth.
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The Archean is the name of the age which began with the forming Earth, as illustrated in this picture.
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Chapter 5 The evolution of life and the biosphere - diversity and complexity, the archean era: the age of bacteria, the proterozoic era: new forms of complexity, the Cambrian explosion: from the microcosm to the macrocosm, mammals and primates, evolution and the earth’s history: “Gaia”, individual species and their histories, summary
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The duration of the Archean, 2.8 billion years, is more than half the expected age of the Earth.
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Although the first continents formed during this eon, rock of this age makes up only 7% of the present world's cratons; even allowing for erosion and destruction of past formations, evidence suggests that continental crust equivalent to only 5-40% of the amount formed during the Archean.[7]
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Although the first continents formed during this eon, rock of this age makes up only 7% of the world's current cratons; even allowing for erosion and destruction of past formations, evidence suggests that continental crust equivalent to only 5-40% of the present amount formed during the Archean.[7]
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