Noah J. Planavsky – författare
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5 produkter
Iron Formations as Palaeoenvironmental Archives
Av Kurt O. Konhauser, Andrey Bekker m. fl.
E-bok, 2022
294 kr
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Ancient iron formations - iron and silica-rich chemical sedimentary rocks that formed throughout the Precambrian eons - provide a significant part of the evidence for the modern scientific understanding of palaeoenvironmental conditions in Archaean (4.0–2.5 billion years ago) and Proterozoic …
Iron Formations as Palaeoenvironmental Archives
Av Kurt O. Konhauser, Andrey Bekker m. fl.
E-bok, 2022
284 kr
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Ancient iron formations - iron and silica-rich chemical sedimentary rocks that formed throughout the Precambrian eons - provide a significant part of the evidence for the modern scientific understanding of palaeoenvironmental conditions in Archaean (4.0–2.5 billion years ago) and Proterozoic …
The Chromium Isotope System as a Tracer of Ocean and Atmosphere Redox
Av Kohen W. Bauer, Noah J. Planavsky m. fl.
Häftad, 2021
308 kr
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The stable chromium (Cr) isotope system has emerged over the past decade as a new tool to track changes in the amount of oxygen in earth's ocean-atmosphere system. Much of the initial foundation for using Cr isotopes (δ53Cr) as a paleoredox proxy has required recent revision. However, the basic …
Chromium Isotope System as a Tracer of Ocean and Atmosphere Redox
Av Devon B. Cole, Christopher T. Reinhard m. fl.
E-bok, 2021
287 kr
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The stable chromium (Cr) isotope system has emerged over the past decade as a new tool to track changes in the amount of oxygen in earth''s ocean-atmosphere system. Much of the initial foundation for using Cr isotopes (δ53Cr) as a paleoredox proxy has required recent revision. However, the basic …
Iron Formations as Palaeoenvironmental Archives
Av Kaarel Mänd, Leslie J. Robbins m. fl.
Häftad, 2022
308 kr
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Ancient iron formations - iron and silica-rich chemical sedimentary rocks that formed throughout the Precambrian eons - provide a significant part of the evidence for the modern scientific understanding of palaeoenvironmental conditions in Archaean (4.0-2.5 billion years ago) and Proterozoic …