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作 者:ISHIWATARI Akira
机构地区:[1]Center for NE Asian Studies,Tohoku Univ.
出 处:《Acta Geologica Sinica(English Edition)》2015年第A02期33-34,共2页地质学报(英文版)
摘 要:Plume-type is a new branch of ophiolite classification introduced by Dilek and Fumes (2011; GSAB, 123,387-). Its most typical example is the komatiite-basalt-gabbro- wehrlite assemblage that is exposed on the Gorgona Island off Colombia, South America and is interpreted as a part of the Caribbean large igneous province (LIP). Analogous rock assemblage occur in the accretionary complexes in the circum-Pacific orogenic belts such as in Japan (Ishiwatari and Ichiyama, 2004; Int.Plume-type is a new branch of ophiolite classification introduced by Dilek and Fumes (2011; GSAB, 123,387-). Its most typical example is the komatiite-basalt-gabbro- wehrlite assemblage that is exposed on the Gorgona Island off Colombia, South America and is interpreted as a part of the Caribbean large igneous province (LIP). Analogous rock assemblage occur in the accretionary complexes in the circum-Pacific orogenic belts such as in Japan (Ishiwatari and Ichiyama, 2004; Int.
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