8. THE OXYGEN ISOTOPIC COMPOSITION OF INTERSTITIAL WATERS: EVIDENCE FOR FLUID FLOW AND RECRYSTALLIZATION IN THE MARGIN OF THE GREAT BAHAMA BANK

ABSTRACT

INTRODUCTION

TECHNIQUES

RESULTS

DISCUSSION

Evidence for the Flushed Zone

Origin of the Increase in Chloride with Depth

Carbonate Diagenesis

CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

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