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pro vyhledávání: '"Urmidola Raye"'
Publikováno v:
Geochimica et Cosmochimica Acta. 164:205-220
The Sokoman Formation is a ca. 100-m-thick succession of interbedded iron formation and fine-grained siliciclastics deposited at 1.88 Ga. Accumulation occurred on a dynamic paleoshelf where oxygen stratification, coastal upwelling of hydrothermally d