大理岩
- marble;griotte
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C岩组主要是一套大理岩,偶有片麻岩。
The lithology of C petrofabric is marble , accidental gneiss .
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大理岩冲击脆断的CT观察研究
CT observation for brittle - shock fracture surface of marble
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基于SEM的大理岩单轴受压全过程细观损伤量化研究
SEM-Based Investigation on the Quantification of Meso-Damage of Marble under Uniaxial Compression
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砂岩和大理岩纵波速度及Q值实验研究
An experimental study of compressive wave velocity and Q value of sandstone and marble
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加载速率对大理岩动态断裂韧度(K(1d))的影响
Influence of loading rate on dynamic fracture toughness of marble
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碳酸盐岩石变质流体中CO2活度的估算方法&以内蒙古集宁群大理岩为例
A method for estimating activity of CO_2 in metamorphic fluids of carbonate rocks & Exemplified by marble of Jining Group in Inner Mongolia
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研究了单轴压缩下超声P波在干燥和饱水的小浪底砂岩和房山大理岩中的衰减和速度。
The QP values as well as the velocities Vp of P wave in dry and saturated specimen of Xiaolangdi sandstone and Fangshan marble are studied as functions of axial stresses .
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大理岩动态拉伸强度及弹性模量的SHPB实验研究
Experimental Study for Dynamic Tensile Strength and Elastic Modulus of Marble using SHPB
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大理岩动态劈裂拉伸的SHPB实验研究
An experimental study for the dynamic split tension of marble disc using SHPB
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大别-苏鲁造山带大理岩中榴辉岩包体的锆石U-Pb年龄及其地质意义
Zircon U-Pb Dating of Marble-associated Eclogite in the Dabie-Sulu Orogenic Belt and Its Geological Implications
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设计基于SEM的大理岩细观损伤全程数字化跟踪试验方案,对四川锦屏大理岩试样进行了单轴压缩细观损伤的全程试验。
A whole process digital tracking test scheme of marble meso-damage based on scanning electron microscopy ( SEM ) is designed for the uniaxial compression of a marble sample from Jinping , Sichuan .
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白云质大理岩中碳酸盐矿物的δ13C值也可以用碳酸岩受到海水碳酸盐混染加以解释。
The δ 13C values observed in carbonate and silicate minerals can also be explained by carbonatite assimilated by oceanic carbonate .
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在MTS伺服压机上对不同饱和状态的砂岩、大理岩标本进行了垂直层理和平行层理两个方向的正弦波加载试验,研究了饱和岩石的各向异性及非线性黏弹性行为。
Low-frequency uniaxial stress cycling tests were conducted on sandstone and marble in different saturation condition to find the possible anisotropic and nonlinear behavior .
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利用新近完成的弹性波参数测量系统,我们在静水压力(常压&32MPa)范围内,对不同饱和度砂岩和大理岩的纵波速度和Q值进行了测试。
With the wave parameter testing system , we have tested the P wave velocity and Q value of Sand (?) stone and Marble with various saturation under the hydraulic pressure ( 0.1 32MPa ) .
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并分析了曲线的特点,建立了由Kelvin模型和Maxwell模型串联组成的Burgers大理岩蠕变理论模型,求出了相应的蠕变参数。
The Burgers theoretical model by Kelvin model and Maxwell model is established by analyzing the features of the curve and its parameters are obtained .
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通过对含硼白云质大理岩C、O同位素及B同位素地球化学进行分析显示了该矿床海相沉积碳酸盐岩的特点,地层及矿体中的硼质同来源于深部。
Analyzing the Geochemistry of C 、 O isotopes and B istope in boracic dolomitic marble , it can be seen that the ore is marine sediment carbonate type , that is , the boron in the layer and in the ore came from the depth .
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本中给出了长宽高为180×40×40mm的大理岩试件的典型荷载-切口张开位移曲线和示波照片。
The load-displacement curve of a marble specimen with size of 180 × 40 × 40mm is given in the paper .
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粒径为5mm的粗晶大理岩,试样强度随长度变化不很明显,长径比小于2.5的试样的峰后应力降低过程大体相似。
For the marble blocks of coarse crystal with grain size of 5 mm , the influence of their length on the strength is not apparent .
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与钻爆法相比,由于TBM不产生爆破力,从而使得大理岩力学性能增加,大理岩的抗破坏能力明显增强。
Compared with the drilling and blasting , blasting the TBM does not produce power , so that the increase in the mechanical properties of marble , marble obviously enhanced the anti-sabotage . 3 .
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豫西东秦岭造山带核部杂岩中大理岩Pb-Pb等时线年龄及其地质意义
Pb-Pb dating of marbles from the core complex of East Qinling orogenic belt , western Henan and its geological implication
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样品尺寸为40cm×40cm×20cm,辉长岩、大理岩各4块。
The scale of rock samples is 40 cm × 40 cm × 20 cm . The samples of gabbro and marble is four piece respectively .
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结果表明:在裂纹缓慢扩展阶段,Q值随应力强度因子的增大总体上呈下降趋势,局部有较复杂的变化,反映了大理岩三点弯曲预制裂纹试样衰减的特殊性。
It is found that the Q Value decreases with the increment of the stress intensity factor from the whole Variation trend but the change law of the Q Value with the stress intensity factor is complicated in the partial scope , reflecting the special attenuation characteristic .
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异常高的δ18O值表明M类榴辉岩与围岩-大理岩在变质过程中发生过强烈的氧同位素交换。
In the Rongcheng region , the extremely high δ 18O values of M-eclogite suggest that a strong oxygen isotopic exchange happened between the M-eclogite and its country-rock , marble , during metamorphisms .
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大别地块高压和超高压变质岩带的大理岩的δ13C数值为1‰~6‰,δ18O数值为5‰~23‰。
δ 13 C of the marble occurred in high pressure and ultra high pressure metamorphic rocks belts of Dabie block are 1 ~ 6 per mil , the δ 18 O from 5 to 23 per mil .
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利用RMT-150B岩石力学多功能试验机完成了单轴压缩状态下砂岩、大理岩和花岗岩试件疲劳破坏变形及机理的较为系统的试验研究。
Testing study is made on the fatigue failure and deformation mechanism of sandstone and marble under uniaxial compression condition with rock mechanics test equipment RMT-150B .
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利用直径00mm的分离式Hopkinson杆对大理岩巴西圆盘和平台巴西圆盘试样进行了动态劈裂实验。
The dynamic split tests of marble using both Brazilian disc and flattened Brazilian disc were performed at high strain rate with split Hopkins pressure bar ( SHPB ) of00mm diameter .
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通过在MTS815.03型电液伺服控制试验机上进行试验,得到了大理岩在不同围压下的应力-应变全过程曲线。
Through the experiments on MTS 815.03 electric-hydraulic servo-controlled testing machine , the whole stress-strain curves of marble at confining pressures are drawn .
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有鉴于此,用两种大理岩制作成CCNBD和ISRM1988年建议方法推荐的人字形切槽三点弯曲圆棒(CB)试样,分别在MTS810型材料试验机进行试验。
In view of it , two types of marbles are used to make CCNBD and chevron bend ( CB ) specimen suggested by ISRM in1988.These specimens are tested on the test machine of MTS810 model .
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利用自行研制的UCT-1型蠕变试验装置,采用单调连续加载和分级加载方式,对南阳大理岩进行了单轴压缩蠕变试验研究。
By continuously loading and multi-stage loading , the creep test on Nanyang marble is performed by using the self-developed UCT-1 apparatus of creep test .
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根据T2y6和T2b大理岩以及砂岩的峰前和峰后循环加卸载试验的结果,提出了弹塑性耦合力学模型。
Based on the results of experiments on two kinds of marble ( T2y6 and T2b ) and a kind of sandstone , an elasto-plastic coupling mechanical model is proposed .