Results 181 to 190 of about 6,981 (220)
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The Paleoproterozoic megascopic Stirling biota
Paleobiology, 2007Abstract 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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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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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, 2018Early 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
2016The 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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Halogen composition of Paleoproterozoic oceans
Goldschmidt2023 abstracts, 2023Ray 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.openaire +1 more source
Assembly of the Siberian Craton: Constraints from Paleoproterozoic granitoids
Precambrian Research, 2020T V Donskaya
exaly

