10. GEOTHERMAL REGIME OF THE WESTERN MARGIN OF THE GREAT BAHAMA BANK

ABSTRACT

INTRODUCTION

IN-SITU BOTTOM-HOLE TEMPERATURES AND THERMAL CONDUCTIVITIES OBTAINED DURING LEG 166

THERMAL CONDUCTIVITIES OF LITHIFIED CORE SAMPLES

OBSERVATIONS

DISCUSSION

Thermal Effect of Sedimentation

Influx of Seawater

Temporal Fluctuation of Bottom-Water Temperature

Heat-Flow Variation along the Transect

CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

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