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Titlebook: Evolution of Archean Crust and Early Life; Yildirim Dilek,Harald Furnes Book 2014 Springer Science+Business Media Dordrecht 2014 Archean c

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Roger N. Walsh,William T. Greenoughy of the Precambrian greenstone belts is reminiscent of the Phanerozoic ophiolites, and suggests that the modern plate tectonics operated as far back as the early Archean, albeit perhaps in a different mode.
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https://doi.org/10.1007/978-1-4842-2749-7nally, the removal of continental lithosphere from beneath the eastern part of the craton in the Phanerozoic is briefly examined, since this phenomenon has wider implications for the global preservation of Precambrian crust.
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Precambrian Greenstone Belts Host Different Ophiolite Types,y of the Precambrian greenstone belts is reminiscent of the Phanerozoic ophiolites, and suggests that the modern plate tectonics operated as far back as the early Archean, albeit perhaps in a different mode.
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The Precambrian Geology of the North China Craton: A Review and Update of the Key Issues,nally, the removal of continental lithosphere from beneath the eastern part of the craton in the Phanerozoic is briefly examined, since this phenomenon has wider implications for the global preservation of Precambrian crust.
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Liang Yu,Haiyan Zhou,Jiayi Shao,Djatmikodrical organic-walled (kerogenous) cells. Backed by a large body of supporting evidence of similar age—other microfossils, stromatolites, and carbon isotopic data—it seems clear that microbial life was present and flourishing on the early Earth ~ 3500 Ma ago.
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Recycling of Lead at Neoarchean Continental Margins, old (> 3.2 Ga) continental margins (OCM) encompassing fragments of Paleo- and Eoarchean protocrust provided the high- or low-µ Pb isotope signatures, depending on the age and U/Pb ratio of the crustal lead sources.
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