Aqueous fluids and sedimentary melts as agents for mantle wedge metasomatism, as inferred from peridotite xenoliths at Pinatubo and Iraya volcanoes, Luzon arc, Philippines
Aqueous fluids and sedimentary melts as agents for mantle wedge metasomatism, as inferred from peridotite xenoliths at Pinatubo and Iraya volcanoes, Luzon arc, Philippines
复制标题
水流体和沉积熔体作为地幔楔交代作用的媒介，根据菲律宾吕宋岛皮纳图博火山和伊拉亚火山的橄榄岩捕虏体推断
作者：
Yoshikawa M;Tamura A;Arai S;Kawamoto T;Payot BD;Rivera DJ;Bariso EB;Mirabueno MHT;Okuno M;Kobayashi T
