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石英压力计的
相关语句
  quartz pressure gauge
     Design and Application of the Small Diameter Quartz Pressure Gauge
     小直径石英压力计的设计与应用
短句来源
  “石英压力计的”译为未确定词的双语例句
     P T calculations suggest maximum M 1 metamorphic conditions of  ̄870℃ and  ̄0.95GPa according to garnet orthopyroxene thermometer and garnet orthopyroxene plagioclase quartz barometer.
     石榴石-斜方辉石温度计及石榴石-斜方辉石-斜长石-石英压力计的计算表明M1变质作用最大的P-T条件为0.95GPa和870℃。
短句来源
     For design of pressure measure interface, a new way is showed which uses quart pressure transducer to measure pressure and uses FPGA to handle output data of quart pressure transducer, it has enhance precision of pressure measure greatly.
     对于压力参数测量接口电路的设计,本文提出了利用石英压力计进行压力测量并使用FPGA对石英压力计的输出值进行处理的解决方法,大大提高了压力测量精度。
短句来源
     As an example of application to the sillimanite-garnet-cordierite gneiss of granulite facies from the Helanshan Group of southern Inner Mongolia, the estimate of Aranovichs geothermobarometer is consistent with that obtained by means of garnet-cordierite Fe-Mg exchange reaction geothermometer and garnet-plagioclase-sillimaaite-quartz geobarometer.
     以内蒙古南部贺兰山群的麻粒岩相矽线石榴堇青片麻岩的温压计算为例,用Aranovich等人实验标定的温压计计算结果与石榴石-堇青石Fe-Mg交换反应温度计和石榴石-斜长石-矽线石-石英压力计的计算结果相当吻合;
短句来源
     Based on measuring principle of stress pressure tool and quarts pressure tool, the calibration principle and method of two kinds of pressure tool was discussed, The mathematical model used to process calibration data was given out.
     文章简述了应变压力计和石英压力计的测量原理,探讨了两种压力计刻度的基本原理和方法,给出了压力计刻度数据处理的数学模型。
短句来源
  相似匹配句对
     Design and Application of the Small Diameter Quartz Pressure Gauge
     小直径石英压力计的设计与应用
短句来源
     Methods to Achieve High Accuracy and Resolution for Quartz Crystal Pressure Gage
     石英晶体压力计的高精度和高分辨率实现方法
短句来源
     Quartz crystal sensor
     石英晶体传感器
短句来源
     Quartz Crystal Oscillators
     石英晶体振荡器
短句来源
     THE SENSITIVITY OF MANGANIN STRESS GAUGE
     锰铜压力计的灵敏度
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This paper briefly reviews the study history of cordierite-garnet-silliman-ite-quartz geothermobarometer, and then introduces an experimentai calibration by Aranovich et al. As an example of application to the sillimanite-garnet-cordierite gneiss of granulite facies from the Helanshan Group of southern Inner Mongolia, the estimate of Aranovichs geothermobarometer is consistent with that obtained by means of garnet-cordierite Fe-Mg exchange reaction geothermometer and garnet-plagioclase-sillimaaite-quartz geobarometer....

This paper briefly reviews the study history of cordierite-garnet-silliman-ite-quartz geothermobarometer, and then introduces an experimentai calibration by Aranovich et al. As an example of application to the sillimanite-garnet-cordierite gneiss of granulite facies from the Helanshan Group of southern Inner Mongolia, the estimate of Aranovichs geothermobarometer is consistent with that obtained by means of garnet-cordierite Fe-Mg exchange reaction geothermometer and garnet-plagioclase-sillimaaite-quartz geobarometer. The estimate of the Hutchesons geothermometer, however, differs from others and thus is in contradiction to the metamorphic condition of granulite facies.

本文简略回顾了堇青石-石榴石-矽线石-石英地质温压计的研究历史,并介绍由Aranovich等人完成的最新实验研究。以内蒙古南部贺兰山群的麻粒岩相矽线石榴堇青片麻岩的温压计算为例,用Aranovich等人实验标定的温压计计算结果与石榴石-堇青石Fe-Mg交换反应温度计和石榴石-斜长石-矽线石-石英压力计的计算结果相当吻合;而应用含有假定的热力学参数的哈奇森的温压计与其它温压计计算结果有较大差别,温度明显偏低,与岩石形成于麻粒岩相变质条件这一地质事实不符。

The stress histories of aluminum plates with different thicknesses induced by a Q -swiched Nd -glass laser beam of pulse duration 70ns and flux of 107 ~ 108W/cm2 measured with a piezoelectric transducer of x -cut quartzcrystul of 10mm in diamerer and 1.2mm or 2mm in thickness. The spot diameter on the samples front was 10mm. The experimental results show that the peak stress σmax is proportional approximately to the square of laser bear flux I2 for I=(3 ~7)J/cm2. The scaling of σmax vs the propagation distance...

The stress histories of aluminum plates with different thicknesses induced by a Q -swiched Nd -glass laser beam of pulse duration 70ns and flux of 107 ~ 108W/cm2 measured with a piezoelectric transducer of x -cut quartzcrystul of 10mm in diamerer and 1.2mm or 2mm in thickness. The spot diameter on the samples front was 10mm. The experimental results show that the peak stress σmax is proportional approximately to the square of laser bear flux I2 for I=(3 ~7)J/cm2. The scaling of σmax vs the propagation distance x seems tobe σmax∝x-(1.02~1.29). An analytical calculation identifies the hot -elastic mechanism of the laser induced stress wave in the aluminum targets herein.

采用两种尺寸全电极式的x切割石英压力计,测量了自由入射面加K_8玻璃窗口两种状态下不同厚度(0.5~4.0mm)铝靶背面的应力应变过程。入射激光波长1.06μm、脉宽20 ns、平均功率密度10~7~10~8W/cm~2、会聚光斑直径8mm。结果表明:激光脉宽不变时,能量密度I愈大,应力波峰压σ_(max)愈高,σ_(max)∝I~2;当I=3~7J/cm~2时,应力波峰值压力与传播距离x的定标关系为:σ_(max)∝x~(-(1.02~1.29));测得应力波形状与解析计算相吻合,证实了在上述光强范围内激光在铝靶中产生应力波的热弹性机制。

Granulite facies pelitic gneiss and mafic granulite outcropping in the Larsemann Hills, East Antarctica, underwent a complicated deformational metamorphic history. Early remnant D 1 structures represent a prograde thickening event which probably formed at 1000Ma (Grenvillian). In response to D 1, M 1 peak metamorphic assemblages were characterized by inclusions of cordierite and sillimanite within coarse grained garnets or spinels in pelitic gneisses and inclusions of orthopyroxene and plagioclase within...

Granulite facies pelitic gneiss and mafic granulite outcropping in the Larsemann Hills, East Antarctica, underwent a complicated deformational metamorphic history. Early remnant D 1 structures represent a prograde thickening event which probably formed at 1000Ma (Grenvillian). In response to D 1, M 1 peak metamorphic assemblages were characterized by inclusions of cordierite and sillimanite within coarse grained garnets or spinels in pelitic gneisses and inclusions of orthopyroxene and plagioclase within coarse grained garnet in mafic granulites. Sapphirine magnetite and sapphirine spinel sillimanite magnetite quartz assemblages included in coarse grained orthopyroxene in orthopyroxene biotite bearing quartzite from Stornes Peninsula have been found, whilst fine grained spinel occurs as inclusions within this sapphirine. P T calculations suggest maximum M 1 metamorphic conditions of  ̄870℃ and  ̄0.95GPa according to garnet orthopyroxene thermometer and garnet orthopyroxene plagioclase quartz barometer. These remnant mineral associations indicate that their metamorphism takes on characteristics of anticlockwise near isobaric cooling (IBC) P T evolution, also reflect a prograde metamorphic formation process of prograde heating during burial. The M 1 (1000Ma) anticlockwise (IBC) P T path derived here for this area may be related to magmatic underplating beneath existing continental crust and intrusion and crystallization of substantial volumes of igneous material within crust. This type of anticlockwise P T path is distinct from the late clockwise P T path evolved during the 500Ma (Pan African).

东南极拉斯曼丘陵出露的麻粒岩相泥质片麻岩和镁铁质麻粒岩经历了复杂的变形变质历史。代表前进的增厚事件的早期残留变质构造D1形成于1000Ma(Grenvilian)期间。对应于D1的变质峰期M1的变质组合以泥质片麻岩的石榴石和尖晶石变斑晶中的堇青石和夕线石包裹体以及镁铁质麻粒岩的石榴石变斑晶中的斜方辉石和斜长石包裹体为特征。在该区斯托尼斯半岛的紫苏黑云石英岩的粗粒紫苏辉石中发现了包裹的假蓝宝石+磁铁矿和假蓝宝石+尖晶石+夕线石+磁铁矿+石英组合,这种假蓝宝石又包裹更细粒的尖晶石包裹体。石榴石-斜方辉石温度计及石榴石-斜方辉石-斜长石-石英压力计的计算表明M1变质作用最大的P-T条件为0.95GPa和870℃。这些早期残留的矿物组合指示了其变质作用具有逆时针近等压冷却(IBC)的P-T演化特征,反映了它们的形成是一个埋深期间前进加热的进变质作用过程。本文得出该区M1(1000Ma)变质作用的逆时针(IBC)P-T轨迹可能与已存在的大陆壳下面的岩浆底侵作用及地壳内大量岩浆物质的侵入和结晶作用有关。此类型逆时针P-T轨迹不同于该区在晚期500Ma(Pan-African)期间顺时针演化的P-T轨迹

 
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