New paper: Some disequilibrium during serpentinization breakdown!

A new article has just been published in Terra Nova journal. Surprisingly, we have demonstrated that the dehydration of serpentinites within the Bergell contact aureole is marked by a strong textural and isotopic (oxygen) disequilibrium. This suggested that rampant disequilibrium is present throughout the contact aureole which make difficult to interpret geochemical change related to metamorphic reactions.




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