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Could peridotite hydration reactions have provided a contributory driving force for Cenozoic uplift and accelerated subsidence along the margins of the North Atlantic and Labrador Sea?
peridotite hydration reactions contributory driving force Cenozoic uplift accelerated subsidence
2009/12/2
This study evaluates the hypothesis that peridotite hydration reactions (e.g.serpentinisation) at the landward termination of transform fracture zones provide a contributory driving force for coupled ...