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

Publisher： John Wiley & Sons Inc

E-ISSN： 2156-2202|86|B4|2737-2755

ISSN： 0148-0227

Source： Journal Of Geophysical Research, Vol.86, Iss.B4, 1981-04, pp. : 2737-2755

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