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xenoliths相关的网络例句

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According to cpx-melt equilibrium pressure, the xenoliths types and simulating calculating of host rock REE partition pattern, source of sodic basalts is garnet lherzolite mantle, and the source of potassic basalt is metasomatic fluid altered phlogopite-containing garnet lherzolite mantle. For the alkaline basalts to sub-alkaline basalts, the melting degrees of the source rocks are 4%~15%.

根据单斜辉石—熔体平衡压力计算、所携带的包体类型及玄武岩稀土元素配分曲线的非实比部分熔融定量模拟表明,钠质玄武岩的来源为石榴石二辉橄榄岩源区,五大连池钾质玄武岩的源区是被交代的含金云母石榴石二辉橄榄岩源区,研究区碱性玄武岩到亚碱性玄武岩是石榴石二辉橄榄岩源区经4%~15%部分熔融程度的产物。

Mafic, ultramafic and/or alkaline volcanic rocks and their entrained mantle peridotitic xenoliths and xenocrysts are known as samples directly from the lithospheric mantle.

基性、超基性火山岩捕获的地幔橄榄岩捕虏体和捕虏晶是直接源自岩石圈地幔的样品。

In comparison with such orthopyroxene in these mantle samples, the secondary orthopyroxene in the Pali Aike xenoliths contains relatively high Ti and Al and low Mg.

与这些环境中地幔样品的斜方辉石相比,Pali Aike 地区的次生斜方辉石含有相对高的Ti和Al,以及相对低的Mg。

Nominally anhydrous minerals, clinopyroxene, orthopyroxene and olivine, in peridotite xenoliths hosted by Cenozoic basalts from Panshishan, Lianshan and Fangshan of the Subei basin, eastern China have been investigated by Micro-FTIR for their water contents.

对来自苏北盆地盘石山、练山和方山地区新生代玄武岩中的50个橄榄岩包体矿物进行了系统的微区傅立叶变换红外光谱分析。

The peridotitic xenoliths can be divided into two groups based on their compositions, namely, the H-type and L-type.

不同颗粒大小的同种矿物之间存在明显的成分差别。

The peridotitic xenoliths can be divided into two groups based on their composition s, namely, the H-type and L-type.

根据橄榄岩的化学成分特征可以将其分为两类: H 型橄榄岩和 L 型橄榄岩。

These peridotitic xenoliths show clear deformed textures and their major minerals show excellent orientation.

橄榄岩捕虏体具有明显的的变形结构,矿物定向排列,属于典型的变形橄榄岩。

Based on detailed studies of petrographic characteristics and major elements of minerals, the authors analyzed trace elements of Cpx in the peridotitic xenoliths from Jining area, Inner Mongolia.

在详细岩相学特征和组成矿物主元素分析基础上,重点对内蒙古集宁玄武岩中橄榄岩包体的单斜辉石进行了激光原位微量元素研究。

Abundant peridotitic xenoliths had been found in the Dashihe Cenozoic basalts in Jiaohe of Jilin Province, northeastern China.

吉林省蛟河市境内大石河新生代玄武岩中含有丰富的地幔橄榄岩包体,详细的岩石学与矿物学研究显示,这些包体的主要岩石类型为尖晶石二辉橄榄岩-方辉橄榄岩,未发现石榴石橄榄岩。

These peridotitic xenoliths show clear deformed textures and their major minerals show excellent orientation. Thus, these peridotites are typical deformed peridotites.

橄榄岩捕虏体具有明显的的变形结构,矿物定向排列,属于典型的变形橄榄岩。

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