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calc-sinter相关的网络例句

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The second intrusive rocks (the representative rocks: Tiantangzhai and Jiuzihe granites) are high-k calc-alkaline and a few are shoshonite rock series, Tiantangzhai and Jiuzihe intrusive rocks show respectively metaluminous and transitional charaterastics between metaluminous and peraluminous.

第二期侵入岩(以天堂寨、九资河侵入岩为例)为亚碱性的钙碱性岩系,多数属于高钾钙碱性岩系,少数为钾玄岩系。

The rocks are potassium-high (K2O=4.10%~5.27%, 4.86% on average) and alkali-rich (Na2O+ K2O=7.12%~8.24%, 7.85% on average) ones, and have an average K2O/Na2O value of 1.63, ACNK values of 0.90~1.05 (0.96 on average) and KN/A values of 0.71~0.89 (0.78 on average), thus belonging to metaluminous to weakly peraluminous granitoids of shoshonite series and K-high calc-alkaline series.

岩石高钾、富碱,K2O含量为4.10%~5.27%,平均4.86%;Na2O+K2O为712%~8.24%,平均7.85%;K2O/Na2O值平均为163;ACNK值在0.90~1.05之间,平均为0.96;KN/A在0.71~0.89之间,平均为0.78,属钾玄岩系列与高钾钙碱性系列准铝质-弱过铝质花岗岩类。

These subvolcanics, in which basalt, basaltic andesite and andesite are dominant, are petrochemically of calc alkaline affinity of subalkaline series and sodic type, and tend to have moderate low total REE, being LREE enriched.

岩石化学上属亚碱性系列、钙碱性火山岩系、钠质类型;稀土总量中低,属轻稀土富集型,稀土分布模式为右倾平滑曲线或略有正、负铕异常;过渡族元素球粒陨石标准化曲线形态呈&W&型,锶初始值为 0 。70 5398,反映物质来源较深。

This module is integrated into large thermochemical database systems such 〓, Thermo-Calc, HSC etc.

但由于受经典化学图绘制的局限,化学位图绘制尚存在很大的不足。

In the K-Na-Ca diagram, intermediate part has the tendency of toellite, and acid part has the tendency of calc-alkaline. According to the above data, its tectonic setting is thought to be continental arc.

其序列组成为石英闪长岩-花岗闪长岩/斜长花岗岩/英云闪长岩-二长花岗岩组合,二长花岗岩略多,地球化学特征具典型造山花岗岩特征,K-Na-Ca图解中性段具英云闪长岩趋势,酸性段呈钙碱性趋势,其构造坏境为大陆弧。

Dalaoling and Xiaofeng suites, belonging to calc-alkaline series, are late-tectonic granitoids emplaced at the brittle domain (5 and .5 km in depth respectively) formed during rapid uplift of the crust.

钙碱性系列的大老岭和晓峰岩套则是在本区地壳迅速隆起过程中分别在5km和<1.5km深度的脆性域定位的构造晚期花岗岩。

The implant material is osteo conductive and can be resorbed via the following two processes: physiological solution in body fluids and direct cellular attack.

calc-i-oss 由高纯度可吸收的β-磷酸三钙组成。这种移植材料具有骨传导性,能够通过以下两种途径被再吸收:体液和直接细胞攻击的生理解决方案。

The high Mg^# calc-alkaline and high Mg^# shoshonitic series in Qiangtang-Mangkang area indicate some intracontinental subduction happened ever in the middle part of the plateau, then the subducted slab broke off and asthenosphere was upwelled 30Ma ago, while the lithospheric mantle was melt to form low Mg^# peralkaline potassic, ultrapotassic series.

综合地球物理资料,提出青藏高原在印度大陆岩石圈的强力楔入下,高原内部软流圈物质沿欧亚岩石圈地幔俯冲板片的顶部向北东和南东挤出,使上覆岩石圈地幔发生剪切破裂,形成一系列串珠状高速体与低速体的相间分布,并随时间不断向北扩展。

The petrological study and studies in element and isotopic geochemistry indicate that the pluton belongs to high-potassium calc-alkaline I-type granite, whose magma came from basic basalt in the thicken crust bottom by partial melting, and are of syn-collisional features. The pluton provides a direct petrological evidence of the plate collision and amalgalation.

岩石学、元素和同位素地球化学研究表明,岩体属于高钾钙碱性Ⅰ型花岗岩,岩浆来源于加厚地壳底部基性玄武质岩石的部分熔融作用,属同碰撞型花岗岩,是板块碰撞拼合的直接岩浆岩证据。

You can also modify these toolbars, as discussed in Chapter 14 (Setting up and Customizing Calc).

您还可以修改这些工具栏,相关的详细内容请参看第14章

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