机译:超俯冲蛇绿岩中透闪石-蛇纹石脉的板状成因:以橄榄石岩浆(新喀里多尼亚)为例
Univ New Caledonia Inst Sci Exactes & Appl BP R4 Noumea New Caledonia;
Univ Rennes 1 CNRS UMR 6118 Geosci Rennes Rennes France;
Univ New Caledonia Inst Sci Exactes & Appl BP R4 Noumea New Caledonia|Bur Rech Geol & Min Orleans France|DIMENC New Caledonia Geol Survey Noumea New Caledonia;
Bur Rech Geol & Min Orleans France;
DIMENC New Caledonia Geol Survey Noumea New Caledonia;
Univ Clermont Auvergne CNRS IRD OPGC Lab Magmas & Volcans F-63000 Clermont Ferrand France;
Univ Lorraine CNRS GeoRessources Fac Sci & Technol F-54506 Vandoeuvre Les Nancy France;
Univ Strasbourg IPGS EOST CNRS UMR 7516 Strasbourg France;
Ophiolite; Tremolite; Antigorite; Veins; Metasomatism; Supra-subduction; Dykes;
机译:岩浆断裂,流体流动和静脉矿化在次胶层区:从TROODOS Ophiolite和Izu-Bonin Forearc和后弧的静脉胶质钙的比较研究
机译:铁同位素行为在北西藏北部胶片区异丙石的熔体恒星相互作用期间
机译:Ophiolite Hosed Chromitite通过Supra-俯冲区橄榄石 - 平面相互作用形成
机译:A'Nyemaqen Ophiolite阶下持续的Dur'ngoi巨大Cu-Co-Zn硫化物矿床成因初步研究,昆汉MT,Kunhin MT
机译:俄勒冈州西南部的塞克斯顿山区:构造胶结的侏罗纪超俯冲带蛇绿岩复合体。
机译:通过板坯衍生的金属熔体形成超低速区的起源
机译:岩浆断裂,流体流动和静脉矿化在次胶层区:从TROODOS Ophiolite和Izu-Bonin Forearc和后弧的静脉胶质钙的比较研究