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      An oxygen isotope profile in a section of Cretaceous oceanic crust, Samail Ophiolite, Oman: Evidence for δ18O buffering of the oceans by deep (>5 km) seawater-hydrothermal circulation at mid-ocean ridges

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      Journal of Geophysical Research: Solid Earth
      American Geophysical Union (AGU)

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          Submarine thermal sprirngs on the galapagos rift.

          The submarine hydrothermal activity on and near the Galápagos Rift has been explored with the aid of the deep submersible Alvin. Analyses of water samples from hydrothermal vents reveal that hydrothermal activity provides significant or dominant sources and sinks for several components of seawater; studies of conductive and convective heat transfer suggest that two-thirds of the heat lost from new oceanic lithosphere at the Galápagos Rift in the first million years may be vented from thermal springs, predominantly along the axial ridge within the rift valley. The vent areas are populated by animal communities. They appear to utilize chemosynthesis by sulfur-oxidizing bacteria to derive their entire energy supply from reactions between the seawater and the rocks at high temperatures, rather than photosynthesis.
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            The oxygen isotope geochemistry of igneous rocks

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              World-Wide Correlation of Mesozoic Magnetic Anomalies, and Its Implications

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                Author and article information

                Journal
                Journal of Geophysical Research: Solid Earth
                J. Geophys. Res.
                American Geophysical Union (AGU)
                01480227
                April 10 1981
                April 10 1981
                : 86
                : B4
                : 2737-2755
                Article
                10.1029/JB086iB04p02737
                217c6aec-3c4a-4d54-8c47-67ba2f99c7b6
                © 1981

                http://doi.wiley.com/10.1002/tdm_license_1.1

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