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- [32] AN OXYGEN ISOTOPE PROFILE IN A SECTION OF CRETACEOUS OCEANIC-CRUST, SAMAIL OPHIOLITE, OMAN - EVIDENCE FOR DELTA-18-O BUFFERING OF THE OCEANS BY DEEP (LESS-THAN 5 KM) SEAWATER-HYDROTHERMAL CIRCULATION AT MID-OCEAN RIDGES JOURNAL OF GEOPHYSICAL RESEARCH, 1981, 86 (NB4): : 2737 - 2755