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

Author:

Gregory Robert T.,Taylor Hugh P.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference74 articles.

1. Oxygen isotope geothermometry of mafic igneous rocks;Anderson;J. Geol.,1971

2. Dilemma of a Cretaceous time scale and rates of sea-floor spreading;Baldwin;Geology,1974

3. Barker , P. F. Initial Reports of Deep Sea Drilling Project 36 U.S. Government Printing Office Washington, D. C. 1976

4. Present day serpentinization in New Caledonia, Oman and Yugoslavia;Barnes;Geochim. Cosmochim. Acta,1978

5. Oxygen isotope geochemistry of the Abitibi greenstone belt, Ontario: Evidence for seawater/rock interaction and implications regarding the isotopic composition and evolution of the ocean and oceanic crust;Beaty;Geol. Soc. Amer. Abstr. Programs,1979

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