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At Site 449, middle Miocene carbonate oozes overlie older pelagic clays deposited below the CCD. This anomalous sedimentation is attributed to an uplift of the site with displacement of at least 200 meters. The vertical tectonism occurred about 15 m.y. ago, roughly synchronous with the cessation of spreading in the Parece Vela Basin and with strong volcanic activity on the West Mariana Ridge. Uplifts of crustal sectors concurrent with the end of spreading and strong volcanic phases might be common in back-arc basins.

Tectonic Significance of the Sedimentary Column at Site 449 (Western Parece Vela Basin), Deep Sea Drilling Project Leg 59