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granitic相关的网络例句

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In addition, the porphyritic allanite- formed by magmatic crystallization was found in the granitic gneisses, it not only shows that the granitic gneisses were metamorphized from magmatic rocks, but also shows that the degree of the metamorphism undergoen was not very intense.

另外在花岗片麻岩中发现有岩浆结晶成因型褐帘石斑晶的残留,这一方面说明这套花岗片麻岩的原岩是种岩浆岩,同时说明它们所经历过的变质作用程度不可能很强。

In this paper the author report deals the type and features of granitic geomorphologic landscape in Chaya Mountain National Geopark. Contrast features of granitic geomorphologic landscape of Mt. Chaya to with those of granitic geomorphologic landscape in China and in the world,Features of granitic geomorphologic landscape Mt. Chaya:①granitic geomorphologic landscape are mainly pictographic stones of granitic geomorphologic landscape ,which have a hundred and tens for pictographic stones of granite in Chaya Mountain.

本文论述嵖岈山国家地质公园花岗岩地貌景观的类型、花岗岩地貌景观特征,对河南遂平嵖岈山花岗岩地貌景观特征与国内外典型花岗岩地貌景观进行了对比分析,嵖岈山花岗岩地貌景观特征:①嵖岈山花岗岩地貌景观主要是花岗岩像形石地貌景观,各种形态的花岗岩像形石有100多个。

We think that feature of granitic geomorphologic landscape of Mt. Chaya, which had been formed by syenogranite with medium—coarse grains,mineral crystallized more coarse and equal,joint and fissure of productional are even spacing,unique geomorphologic place and the special climate condition is from north subtropical zone to warm temperate zone, are evidence that granitic geomorphologic is marked zone.

认为嵖岈山花岗岩地貌景观的特征是因嵖岈山花岗岩为中粗粒正长花岗岩,矿物颗粒结晶比较粗且岩性较均一、岩体内节理裂隙发育程度疏密适中、独特的地貌部位和北亚热带向暖温带过渡地带的气候条件形成的,是花岗岩地貌显著地带性有力见证。

Based on the study of the ages, mineral chemical, petrochemical and isotopic geochemical characteristics of granitic gneisses in Shuihou area of southern Dabie mountain, combining with the study of comparing these gneisses with the orthogneisses in northern Dabie mountain, it can be fould that there were clearly differentices between the granitic gneisses in southern Dabie and northern Dabie mountain.

论文通过对该造山带南大别水吼地区花岗片麻岩的时代、矿物化学、岩石化学及同位素地球化学特征的综合研究,并通过与北大别正片麻岩的对比研究,进一步证实南、北大别的花岗片麻岩套具有明显的差别。

By contrasting compositistion and analysis of granitic normal weight , rare-earth and trace elements , it is used to judge the origin and structure environment of granitic.

通过对该区花岗岩的常量元素、稀土元素及微量元素成分进行分析和对比研究,对花岗岩的成因及形成的构造环境进行了综合判别。

This paper discusses four series of red, black, green and white granitic rocks, which include more than ten kinds of granitic rocks.

本文讨论了朱阳地区红、黑、绿、白色4大系列和十余种花岗岩石材品种。

The garnets in the granitic gneisses from southern Dabie mountain were characterized by riching in Fe and Mn, and pooring in Mg, differing from the garnets in the UHP gneiss and eclogite, which relatively riching Mg. But the plagioclase in the granitic gneisses from the northern Dabie mountain was relative high Ca contenents, their An is 25.2-27.9, within the oligoclase field.

石榴石总体以贫Mg富Fe和富Mn为特征,明显不同于榴辉岩及高压片麻岩中石榴石相对富Mg的情况;而北大别英云闪长质片麻岩中斜长石的钙含量相对较高,An为25.2-27.9,位于奥长石范围内,角闪石中Mg的含量较高,具有壳幔混合源的特征。

The Nanping granitic pegmatite is one of the most important rare-metal deposits in China. In this pegmatite field the No. 31 granitic pegmatite is the most highly evolved and well mineralized one, where beryl is the most important beryllium mineral.

福建南平花岗伟晶岩是中国重要的稀有金属花岗伟晶岩之一,其中31号脉是分异程度最高、稀有金属成矿作用最重要的岩脉,绿柱石是其中最主要的铍矿物。

Based on the study of mineral crystallization sequence, solidus temperature and growth rates of quartz and albite, it suggests that Li_F_Na enriched granitic residual magma is qualified for the formation of snowball texture, and that high_ratio of Na 2O/K 2O and contents of F and H 2O in the granitic melt are important to the formation of snowball texture.

对矿物结晶顺序、石英和钠长石的生长速率以及固相线温度的研究表明,富锂、氟、钠的花岗质残余岩浆完全具备形成雪球结构的条件。

By studying the deformation and evolutionary sequences around the Panshan granitic pluton, east-central Yanshan orogenic belt, and 40 Ar/ 39 Ar thermochronological test and analysis,we present the structural evolutionary process of the overlying strata before pluton intruded as well as it was intruding. The sequences of regional deformation are as follows: before the intrusion of Panshan granitic pluton, the N-S trend contraction in the east-central Yanshan orogenic belt took place, which resulted in the regional EW-trending Malanyu multi-fold and Jixian thrust fault; then Panshan granitic pluton intruded into the south limb of the Malanyu multi-fold and cut-through the Jixian thrust fault; later, the reactivity of the Jixian thrust fault cut off the synclines around thePans han granitic pluton.

通过对燕山东段盘山花岗岩岩体周缘构造变形特征、演化过程的研究,并结合40Ar/39Ar 热年代学测试和分析,提出盘山岩体侵位前、侵位时其上覆岩层的构造演化过程:三叠纪末(210-200 Ma)盘山岩体侵位前,燕山中东段受南北向挤压作用形成了近东西向的马兰峪复背斜和蓟县逆冲断裂;盘山岩体侵位于先期形成的马兰峪复背斜南翼,并侵蚀了蓟县断裂;蓟县断裂的后期再次活动截切了盘山岩体的周缘向斜。

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