36. Serpentinized Peridotite Breccia and Olistostrome on Basement Highs of the Iberia Abyssal Plain: Implications for Tectonic Margin Evolution

ABSTRACT

INTRODUCTION

SUMMARY OF EARLY CRETACEOUS SEDIMENTS AND AGES

PETROLOGY OF BRECCIAS AND MAFIC ROCKS AT SITE 899

FABRICS OF THE SERPENTINIZED PERIDOTITE BRECCIAS AT SITE 899

OLISTOSTROMES

DISCUSSION ON PALEOGEOGRAPHY AND TECTONIC SETTING

CONCLUSION

ACKNOWLEDGMENTS

REFERENCES

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