[1]
Tamura, A., Makita, M. and Arai, S. 1999. ORIGIN OF HIGHLY REFRACTORY PERIDOTITES: IMPLICATIONS FOR DIVERSITY OF HIGH-MG ANDESITE MAGMA GENESIS. Ofioliti. 24, 1b (Mar. 1999), 174-175. DOI:https://doi.org/10.4454/ofioliti.v24i1b.88.