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Solid-state mantle convection coupled with a crystallising basal magma ocean
Fractional crystallisation of a basal magma ocean (BMO) has been proposed to explain the formation of large scale compositional variations in the mantle and the persistence of partially molten patches in the lowermost mantle. We present a complete set of
Labrosse, Stéphane+2 more
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Cauchy Integral of Calderón on the Graphs of Functions with BMO Derivatives [PDF]
Kôzô Yabuta
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SOME EMBEDDINGS RELATED TO HOMOGENEOUS TRIEBEL–LIZORKIN SPACES AND THE BMO FUNCTIONS
As the homogeneous Triebel–Lizorkin space $\dot{F}_{p,q}^s$ and the space BMO are defined modulo polynomials and constants, respectively, we prove that BMO coincides with the realized space of $\dot{F}_{\infty, 2}^0$ and cannot be directly identified ...
B. Gheribi, M. Moussai
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𝐿^{∞}-BMO boundedness for a singular integral operator [PDF]
Javad Namazi
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Sobolev embeddings into BMO, VMO, and L∞ [PDF]
Andrea Cianchi, Luboš Pick
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