Metasomatism in Oceanic and Continental Lithospheric Mantle: introduction
Gregoire M., COLTORTI, Massimo
core
Breakup of strong cratonic lithosphere causes extensive magmatism at continental margins. [PDF]
Wang S, Leng W.
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Asynchronous transfer of magmas and mineralizing fluids in a plutonic-subvolcanic-volcanic plumbing system. [PDF]
Paoli G +4 more
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Petrologic evidence for core sulfur degassing in partially differentiated planetesimals. [PDF]
Wang SZ +5 more
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Melt flow control on lithological and geochemical heterogeneity of the oceanic upper mantle. [PDF]
Rui HC +9 more
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Redox state of subducted sediments controls porphyry copper mineralization along the Tethyan belt. [PDF]
Li H, Yang Z, Lu Y, Hou Z.
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Mantle-derived morphologies of diamond: records of diamond-destroying mantle metasomatism
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A tale of two planets: Disparate evolutionary models for Mars inferred from radiogenic isotope compositions of Martian meteorites. [PDF]
Borg LE, Kruijer TS.
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Mobilization of isotopically heavy sulfur during serpentinite subduction. [PDF]
Schwarzenbach EM +8 more
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Periodic instability and restoration of cratonic lithosphere. [PDF]
Liu L +5 more
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