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By studying the occurance of gold orebodies,the ore types and features and the alteration of wall rocks ,it is found that Xuyaogou gold deposit is a quartz vein-metasomatite type locating in the exocontact zone of Muhuding granodiorite.

通过对许窑沟金矿床矿体产出特征、矿石类型及特征、金的赋存状态以及围岩蚀变等的研究表明,许窑沟金矿是赋存于牧虎顶岩体外接触带的石英脉-蚀变岩型金矿床。

The calculation of the elemental mass balance interprets by elemental calculation to explains the elementary activity law: the composition of alteration rock in the central of alteration belt has the largest degree of variation, a large number of permeability fluid carry active components into the dilation space, which has significance to the further enrichment of the ore-forming element and the remobilization of correlative elements.

通过元素质量平衡计算解释了成矿过程中体系的元素行为规律:蚀变带中心蚀变岩的成分变异强度最大,大量渗透性流体携带活泼组分进进扩容带,对成矿元素进一步富集,相关元素(Ag、Cu、Zn、Hg、Pb)活化转移产生重要的影响。

Based on the characteristics of corrosion metrics and micromechanics ,the paper describes a mechanical property prediction procedure for corroded aluminum alloy.

根据点蚀损伤的特点,在细观力学的理论基础上,建立了点蚀损伤材料弹性性能计算的孔隙率模型。

The relationship between molecular structure of the compound and the inhibition efficiency was investigated by ab i...

同时用量子化学中的从头算方法对缓蚀剂的分子结构与缓蚀性能的关系进行了研究。

By means of electrochemical polarization,the corrosion inhibition effect on copper of sodium molybdate and triethano-lamine was evaluated.

利用极化曲线法研究了钼酸钠以及钼酸钠和三乙醇胺以特定的配比形成的复合缓蚀剂对铜的缓蚀作用。

An investigation on cavitation erosion of nodular cast iron is presented in this paper.

针对球铁的汽蚀特性进行了研究,认为球铁中的石墨是球铁的汽蚀破坏源。

Therefore, the morphology of the etch pits can be predicted, or conversely the orientation of surface can readily be determined from the morphology of etch pits.

指出:利用这一点,在已知晶面的晶格对称性的情况下,可预料蚀坑的形状;或反过来,从蚀坑的形态可很容易判断其所在晶面的取向。

The paper about the studies on alteration-deformation rock mineralogy and geochemistry indicates from unaltered phyllite to ultramylonite, SiO〓, CaO increase, Al〓O〓, TiO〓, TFe, MgO, K〓O decrease, P〓O〓 and MnO〓 almost remains constant, with the deformation degree increase.

蚀变变形岩石学及地球化学研究表明,由未蚀变的千枚岩经糜棱岩到超糜棱岩,随着变形程度的提高,SiO〓、Na〓O含量逐渐增加,Al〓O〓、TiO〓、TFe、MgO、K〓O逐渐减少,而P〓O〓、MnO〓基本保持不变,岩石的密度也逐渐降低。

According to logging results of 167 boreholes and chemical analyses of 24 369 samples as well as characteristics of element distribution at 4 000 m, 3 950 m and 3 900 m levels, the deposit is characterized by alteration, mineralization and element geochemistry of the porphyry. Alteration and mineralization are spatially and temporally related to the augen quartz phenocryst_bearing hornblendequartz diorite porphyrite (J3δομ).

根据167个勘探钻孔编录和化学分析(24369件化学分析样品)资料,以及对海拔4000 m、3950 m、3900 m水平面的Cu、Au、Ag、Mo、Mn、P b、Zn、W、K、Na、Ca、Rb元素分布规律的分析,显示矿体具有斑岩型矿床的蚀变、矿化以及元素地球化学特征,主要矿化和围岩蚀变在时间上和空间上均与含眼球状石英斑晶的角闪石英闪长玢岩(J3δομ)有关。

According to logging results of 167 boreholes and chemical analyses of 24 369 samples as well as characteristics of element distribution at 4000 m, 3950 m and 3900 m levels, the deposit is characterized by alteration, mineralization and element geochemistry of the porphyry. Alteration and mineralization are spatially and temporally related to the augen quartz phenocryst-bearing hornblende-quartz diorite porphyrite (J3δομ).

根据167个勘探钻孔编录和化学分析(24369件化学分析样品)资料,以及对海拔4000m、3950m、3900m水平面的Cu、Au、Ag、Mo、Mn、Pb、Zn、W、K、Na、Ca、Rb元素分布规律的分析,显示矿体具有斑岩型矿床的蚀变、矿化以及元素地球化学特征,主要矿化和围岩蚀变在时间上和空间上均与含眼球状石英斑晶的角闪石英闪长玢岩(J3δομ)有关。

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