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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