Abstract
Important information regarding the evolution of the ocean and climatic changes of the Earth during geological history becomes available from investigating oxygen and hydrogen isotope abundances in pore waters and in the minerals of sedimentary rocks.
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© 2012 Springer Science+Business Media B.V.
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Ferronsky, V.I., Polyakov, V.A. (2012). Hydrogen and Oxygen Isotopic Composition of Sedimentary Rocks of Marine Genesis and Implications for Paleothermometry. In: Isotopes of the Earth's Hydrosphere. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-2856-1_8
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DOI: https://doi.org/10.1007/978-94-007-2856-1_8
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