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- W3152429605 abstract "为了区分主要微观结构，在主人岩浆在捕虏体乘火车以后从第二等的现象在披风条件下面发展了，这研究打算讨论开始多孔，筛粗糙，并且在从西方的诺思中国 craton 的新生代暗岩的披风捕虏体的矿物质谷物上的反应边界。主要 clinopyroxene 上的多孔的边界向主机暗岩显示出既不明显的组合 zoning 也不优先的开发并且当捕虏体向上被带，可能经由在 lithospheric 披风或压力版本以内的部分融化建议起源。在主要尖晶石表演的筛粗糙的边界与向主人暗岩增加 Cr# 和减少的艾尔清除化学 zoning。他们作为由于主人加热玄武岩的岩浆和减少的压力在期间的部分融化的结果被解释上升过程。Post-entrainment 反应主要在在主人之间的接触产生了第二等的矿物质玄武岩融化并且捕虏体。在反应边界的第二等的 clinopyroxene 在主要 clinopyroxene 上发展并且比主要的有更高的 Ti， Ca，和 Fe 内容和 Si 内容，当主要 Cr-Al 尖晶石上的第二等的尖晶石是 titanomagnetite 时。在主要 orthopyroxene 上的反应边界的第二等的橄榄石和 clinopyroxene 在 Fe，艾尔，和 Ti 被充实。在披风捕虏体的反应边界的出现在捕虏体乘火车以后反映不平衡过程在玄武岩融化。主要 clinopyroxene 上的多孔的边界不能与和主人的相互作用有关玄武岩当主要尖晶石上的筛粗糙的边界和主要 clinopyroxene，尖晶石，和 orthopyroxene 上的反应边界可以源于在主人之间的 post-entrainment 反应时，融化玄武岩融化并且捕虏体矿物质。" @default.
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- W3152429605 date "2012-01-01" @default.
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- W3152429605 title "Post-Entrainment Mineral-Magma Interaction in Mantle Xenoliths from Inner Mongolia, Western North China Craton" @default.
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