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The Paleoproterozoic megascopic Stirling biota

Paleobiology, 2007
Abstract The 2.0–1.8-billion-year-old Stirling Range Formation in southwestern Australia preserves the deposits of a siliciclastic shoreline formed under the influence of storms, longshore currents, and tidal currents.
Stefan Bengtson   +2 more
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Isotopic and geochemical constraints on the Paleoproterozoic Hutchison Group, southern Australia: Implications for Paleoproterozoic continental reconstructions

Precambrian Research, 2011
Abstract Geochemical, Sm–Nd isotopic, and U–Pb–Lu–Hf zircon analyses reveal the sedimentary succession formerly recognised as the Hutchison Group consists of three temporally and isotopically distinct groups, divided by a crustal-scale shear zone (Kalinjala Mylonite Zone).
Szpunar, M.   +4 more
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A strongly oxidizing Paleoproterozoic era

Science, 2018
Early Earth Two billion years ago, marine sulfate concentrations were around one-third as high as modern ones, constituting an oxidizing capacity equivalent to more than 20% of that of the modern ocean-atmosphere system. Blattler et al.
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The Paleoproterozoic Eastern Bahia Orogenic Domain

2016
The Paleoproterozoic Eastern Bahia orogenic domain occupies an approximately 200 km-wide area in the northern Sao Francisco craton, located between the Atlantic coast and the interior plateau of Bahia state known as the Chapada Diamantina. Together with its African counterpart, the West Central African belt of Gabon, the Eastern Bahia orogenic domain ...
Johildo Salomão Figueirêdo Barbosa   +1 more
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Neoarchean–Paleoproterozoic supercycles

2021
Johanna Salminen   +3 more
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Halogen composition of Paleoproterozoic oceans

Goldschmidt2023 abstracts, 2023
Ray Burgess   +3 more
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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.
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