Trace elements in clinopyroxenes of peridotites from Mariana forearc seamounts (ODP Leg 195, Site 1200A, and ODP Leg 125, Sites 779A and 784A): Evidence for polybaric, high-degree, fractional mantle melting.

Conference Poster
Publication Date:
2003
Iris type:
04.03 Poster in Atti di convegno
Handle:
https://iris.cnr.it/handle/20.500.14243/437652