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- W3148189711 abstract "二种类型融化衣袋，关门融化衣袋(CMP ) 并且开融化衣袋(OMP ) ，从橄榄岩捕虏体被认出在西方的 Qinling 在新生代 kamafugites 乘火车() ，华中。Haoti () CMP 有 olivine+clinopyroxene+amphibole+K 长石的一个矿物质集合，而 Baiguan () CMP 由 olivine+clinopyroxene+ilmenite+carbonate 组成。OMP 的部件是更复杂的。在 Haoti OMP，有橄榄石， clinopyroxene，玻璃，低形式的许多闪石， K 长石(Kfs ) ，钛铁矿，硫化物，绿泥石， perovskite，铬铁矿和金云母。Baiguan OMP 包含橄榄石， clinopyroxene，玻璃，绿泥石和铬铁矿。组合地，在 CMP 和 OMP 的橄榄石显然两个都在 OMP 在 Ni，和那些被弄空也在 Fe 和 Mg 被弄空，并且与主要的相比在 Ca 充实。Clinopyroxenes 显示在 CMP 和 OMP 之间的大、系统的组合变化特别地在艾尔， Cr， Na， Ca 和 Ti。眼镜通常与世界范围的眼镜相比在 Si 被弄空在融化衣袋，尽管他们仍然有大变化。闪石和 K 长石相对限制了组合变化。petrographical 观察和矿物质化学建议 Haoti 和 Baiguan CMP 被产生由在原处解压缩融化 orthopyroxenes，橄榄石和 clinopyroxenes，并且由次要的外部 K 富有、 Ca 富有的 melt/fluids 的增加。在西方的 Qinling 下面在 lithospheric 披风在最近的交代矿床事件期间形成的 OMP。" @default.
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- W3148189711 date "2010-01-01" @default.
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- W3148189711 title "Formation of Melt Pocket in Mantle Peridotite Xenolith from Western Qinling, Central China： Partial Melting and Metasomatism" @default.
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