Deep subduction, melting, and fast cooling of metapelites from the Cima Lunga Unit, Central Alps
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DOI: 10.1111/jmg.12621
Abstract: The Cima Lunga unit in the Central Alps is dominated by quartzofeldspathic gneisses with subordinate mafic, ultramafic, and metacarbonate rocks. Only mafic and ultramafic lithologies were thought to preserve clear evidence of Alpine high‐P metamorphism.… read more here.
Keywords: lunga unit; cima lunga; central alps; unit ... See more keywords