Melting phase equilibria from 4 to 7 gpa in the system cao-mgo-al2o3-sio2-co2, the persistence of the “ledge“ in carbonated basalt with excess silica, and the most likely limits on the depths of termination of carbon cycle at subduction zones

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• who: Shantanu Keshav et al. from the Universitu00e4t Bayreuth, Bayreuth, Germany, Institute of Earth Sciences, University of Iceland, Reykjavik, Iceland have published the paper: Melting Phase Equilibria from 4 to 7 GPa in the System CaO-MgO-Al2O3-SiO2-CO2, the Persistence of the ``Ledge`` in Carbonated Basalt with Excess Silica, and the Most Likely Limits on the Depths of Termination of Carbon Cycle at Subduction Zones, in the Journal: (JOURNAL) of August/30,/2021
• what: In the paper presented at the 2009 Goldschmidt Conference, Luth remarked that the different high-pressure melting behaviors of . . .
  

   

  

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