8. Distribution of Clay Minerals in Drift Sediments on the Continental Rise West of the Antarctic Peninsula, ODP Leg 178, Sites 1095 and 1096

ABSTRACT

INTRODUCTION

MATERIALS AND METHODS

RESULTS

DISCUSSION

Provenance of Clay Mineral Assemblages

Glacial-Interglacial Cyclicity of Clay Mineral Assemblages during the Late Quaternary

Neogene to Quaternary Clay Mineral Assemblages in Sediments at Sites 1095 and 1096

CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

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