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Showing 1 to 1 of 1 for “"thermochemischer Mantelkonvektion"”.
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Stability of the large low shear velocity provinces
We study segregation of the subducted oceanic crust (OC) at the core mantle boundary and its ability to accumulate and form large thermochemical piles (such as the seismically observed Large Low Shear Velocity Provinces - LLSVPs). Our high-resolution numerical simulations suggest that the longevity …