10. Identification of the Glacial Signal from the Antarctic Peninsula since 3.0 Ma at Site 1101 in a Continental Rise Sediment Drift

ABSTRACT

INTRODUCTION

MATERIALS AND METHODS

RESULTS

DESCRIPTION AND INTERPRETATION OF LITHOFACIES

DISCUSSION

CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

APPENDIX

Data Used to Calculate Mass Accumulation Rates of Coarse-Sand Ice-Rafted Debris at Site 1101

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