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Primary hematite in Neoarchean to Paleoproterozoic oceans

Geological Society of America Bulletin, 2015
Banded iron formations (BIFs) are ironand silica-rich chemical sedimentary rocks formed throughout the Archean and Paleoproterozoic Eras. The presence of hematite (Fe2O3) and magnetite (Fe3O4) in BIFs has led to the widespread assumption that Fe(II) oxidation must have occurred in the ancient oceans via either a biological or chemical mechanism ...
Si Sun   +3 more
openaire   +3 more sources

Neoarchean–Paleoproterozoic supercycles

2021
Johanna Salminen   +3 more
openaire   +1 more source

Halogen composition of Paleoproterozoic oceans

Goldschmidt2023 abstracts, 2023
Ray Burgess   +3 more
openaire   +1 more source

GROWTH AND MODIFICATION OF NEOARCHEAN-PALEOPROTEROZOIC CRUST

The temporal distribution of Earth’s crustal rocks exhibits distinctive age peaks, representing periods of significant crustal growth. Among these, the Neoarchean (2.7-2.5 Ga) and Paleoproterozoic (2.0-1.8 Ga) stand out as major periods of crustal formation in Earth’s early history.
openaire   +1 more source

Zircon U-Pb age and Hf-O isotope evidence for Paleoproterozoic metamorphic event in South China

Precambrian Research, 2006
Yuanbao Wu   +2 more
exaly  

Archean-Paleoproterozoic transition: The Indian perspective

Earth-Science Reviews, 2019
Shuvabrata De   +2 more
exaly  

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