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Lydéric France, Benoit Ildefonse and Juergen Koepke Hydrous magmatism triggered by assimilation of hydrothermally altered rocks in fossil oceanic crust (northern Oman ophiolite) Geochemistry, Geophysics, Geosystems 14

Version of Record online: 1 AUG 2013 | DOI: 10.1002/ggge.20137

Key Points

  • Hydrous magmatism is part of the general mid-ocean ridges lineage
  • Hydrous component is introduced through assimilation of anatectic hydrous melts
  • Processes able to trigger recycling are presented

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