The nephrite in Qinghai occurs within the internal contact zone between granite and marble.
青海软玉产于花岗岩与大理岩的内接触带。
The contact zone width of crane wheel with track is analyzed by plane stress elastic theory.
采用平面应力弹性理论，对吊车车轮与轨道的接触区尺寸进行理论分析。
Important gold ore bodies generally occur in the contact zone of rock bodies and country rocks.
有规模的金矿体一般产在岩体的接触带上。
The contact deposit is controlled by the contact zone, and shows typical features of skarn orebody.
接触带矿体受接触带控制，具矽卡岩型矿体典型特征。
The value is determined by the grinding wheel speed and the fluid film thickness within the contact zone.
它由砂轮的转速及接触区域的液体薄膜的厚度决定。
Temperature response at contact zone during grinding of granite were measured using thermocouple detector.
采用热电偶夹丝法测量了平面磨削山西黑石材过程中接触弧区的温度。
The variation of lateral displacement affects extremely the geometry and mechanics parameters in contact zone.
横移量的变化将极大地影响接触斑上的几何参数和力学参数。
Based on the above straight lines, the contact zone can be determined from the known indentor curvature and loading.
根据这些直线族，可以由已知的压头曲率和外载荷确定接触区尺寸。
The state of tool workpiece contact zone in Electric Hot Machining (EHM) is different from that of conventional cutting.
导电加热切削时，刀工接触区的状态与常规切削的不同。
Therefore, a conclusion might be drawn that the exo-contact zone and nearby was the favorable position for ore formation.
因此，外接触带及其附近的围岩是成矿的有利部位。
A new method is designed for in process monitoring of grinding temperature at contact zone in workshop with strong interference.
设计了一种可以在生产现场的强背景干扰下在线监测磨削弧区温度的新方法。
The contact zone between roller and workpiece and its contour's definition are the cruxes of establishing the FEM mechanical model.
在建立筒形件强旋有限元力学模型过程中，旋轮与工件接触区及其边界的描述是重要的一环。
The spacious outdoor area within the complex will be designed communally and serve as a contact zone for the residents of both buildings.
建筑群宽敞的户外区域将被设计成公共区域，作为两座建筑中的居民的生活交流区。
Daheishan gold deposit is a fractured alteration type and quartz vein type gold deposit, hosted in the outer contact zone of Damiao granite.
大黑山金矿是赋存于大庙花岗岩体外接触带的破碎蚀变岩型和石英脉型金矿。
The grain refinement begins from the center ellipsoidal zone, and then gradually expands to the vertical edge zone and conical contact zone.
细化首先开始于易变形区，再相继扩展到纵向棱边区和接触锥形区。
Ludousou gold deposits belong to fractured altered rock-type gold deposit, produced in Dewulu quartz diorite and Ludousou quartz porphyry contact zone.
录斗艘金矿床属破碎蚀变岩型金矿，产于德乌鲁石英闪长岩与录斗艘石英闪长斑岩接触带附近。
Granite is distributed in the periphery of mining area far from the andalusite bodies, and its contact zone can't control the pegmatitic andalusite bodies.
矿区内未见花岗岩体出露，矿区外围虽有花岗岩体分布，但距离矿体很远，矿体并不受岩体接触带控制。
The scheelite orebody of the Yangjingou mining area occurred in the contact zone of the lower Paleozoic Wudaogou Group strata and the Indo-Sinian adamellite.
杨金沟矿区白钨矿体产于下古生界五道沟群地层与印支期二长花岗岩内外接触带中。
The copper (molybdenum) ore bodies are mainly situated in or out of the contact zone between the mineralized porphyry bodies and the biotite granite porphyry.
铜(钼)矿(化)体主要产于含矿斑岩体和黑云母花岗斑岩的内外接触带中。
Cu-Pb-Zn ore bodies are located in outer contact zone of intermediately acidic granite(partially layered skarn) and the ore occurs as dissemination and fracture-filling.
铜铅锌矿体分布于酸性偏中性的花岗岩体外接触带中（部分为层状夕卡岩），呈浸染状赋于夕卡岩中或沿裂隙充填成矿。
The light coloured nephrite, which formed on the contact zone of the dolomitic marbles and the granites, has more translucency and practically has not ore dissemination.
产于大理岩和花岗岩接触带的浅色软玉，透明度高，无金属矿物浸染。
Marmatite is the guide mineral of the second ore type which appears in bedded, veined and irregular ore bodies near contact zone of magmatic rock or joint positions between faults and ore beds.
另一种以铁闪锌矿为标志，矿体呈似层状、脉状及不规则状等，靠近岩体接触带或断裂与赋矿层的交汇部位产出，代表了成矿第二世代。
The inner, outside contact zone between Himalayan ultra-epizonal syenite porphyry, Indosinian volcanic rocks of liparite porphyry-dacite series and strata is very advantageous to the metallogenesis.
大面积喜马拉雅期超浅成正长斑岩、印支期流纹斑岩英安岩系列火山岩类与地层的内、外接触带对成矿十分有利。
The main characteristics of the skarn are as follows:(1)occurring as bedded, para-bedded in the contact zone between carbonate and microclastic rock, and its occurrence being accordance to the strata;
研究表明该夕卡岩的主要特征为：（1）呈层状、似层状赋存于碳酸盐岩和细碎屑岩接触带，产状与地层一致；
The contact between fluids is usually gradual rather than sharp, forming a transition zone of mixed fluid.
流体间的接触面常常是渐变的而不是突变的，形成一个混合液体的过渡带。
The contact between fluids is usually gradual rather than sharp, forming a transition zone of mixed fluid.
流体间的接触面常常是渐变的而不是突变的，形成一个混合液体的过渡带。
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