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deposits相关的网络例句

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Gave a revaluating of long-range perspection on them in so many proven testimony; made a suggestion that there had superior metallogenic condition and favourable long-range perspection to find three Mississippi Valley Type Lead-Zinc deposits in Kezileitao-Kusilafu of West Kunlun Mountain Region.

认为塔木-卡拉牙斯卡克、阿尔巴勒克、卡兰古-卡拉塔什是西昆仑地区3个最佳的成矿远景区,在西昆仑地区至少可以找到3个大型的密西西比河谷型铅锌矿床,并为今后找矿工作指明了方向。

Through the analysis of the alloy electroplating solution in gradients, the process variables and their relationship between content of manganese in the alloy coating, the optimum process has been obtained, the additive to improve the cathode current efficiency was found; it was found that the deposits with a manganese content 40~60% exhibit excellent corrosion resistance; the corrosion resistance of zinc-manganese alloy coating will be even better after"phosphated"and passivated.

研究发现Na〓SeO〓能显著提高锌锰合金电沉积电流效率。首次用循环伏安法、恒电势电解法、恒电流阶跃法研究了Na〓SeO〓提高电流效率的作用机理。研究发现Na〓SeO〓在锌锰共沉积的条件下在阴极是分两步还原,即:首先在-0.9V处被还原为单质硒,然后在-1.25V处被还原为多硒阴离子。证明了多硒和多硒阴离子都在阴极存在特性吸附

It was found that the photoactivity was not increased as expected after the POM was loaded with Cs , suggesting the difficulty in deposition control,and pores on the surface of the catalyst covered by the deposits.

同时国际上对于钛柱类催化剂研究转向改变不同载体,层材料对于钛柱类材料的光催化性能的影响的研究受到了越来越多的重视。

The gold deposit types are com plicated,can be divided into five types;hydrothermal breccia gold deposit,similar beded disseminated gold deposit in limestone,old karst cave gold deposit,porphyry gold deposit and skarn gold deposit.The form of these gold deposits are related to Tongshi subvoleanie complex.

该区金矿形戚与铜石次火山杂岩体有关,区内金矿类型复杂,可划分为隐爆角砾岩带型金矿、似层状畏染状灰岩中金矿、古溶洞型金矿、斑岩型金矿、矽卡岩型金矿等5种矿化类型。

So we could utilize GIS technology to manage polygenetic data in the database, and made GIS-based mineral resources assessment in Eastern Kunlun Mountain. At first, a regional deposits exploration model was proposed by us.

在此基础上,我们利用GIS技术对东昆仑空间数据库中多源的地学信息进行集中管理,并对东昆仑地区进行基于GIS的矿产资源评价工作。

The author puts forward that the forming of the Shihugold deposit is of the characteristics of multistage geotectonic evolution,multisource ore- forming materials, multiore- controlling factors,multimineralization, multigenesis typle. Controlled by the fault belt, theShihu gold deposit is a polygenetic compound ore deposits which wasformed in the Archean mesometamorphic rock and reconstructed bymixed hydrothermal in Yanshan Epoch. And a related minerogeneticmodel has been set up.

将矿床成矿作用与大地构造演化阶段联系起来,详细地阐述了石湖金矿床的成矿机理,认为矿床的形成具多大地构造演化阶段,多成矿物质来源、多控矿因素、多成矿作用和多成因类型的特点,提出石湖金矿床属产于太古代中级变质岩系、受断裂破碎带控制的燕山期岩浆改造混合热液型多因复成金矿床,并建立了与之相适应的成矿模式图。

Fluorites formed in uranium mineralization period in the Zoujiashan and Shazhou uranium deposits have ε〓 values from -6.7 to -8.3 and I〓 values from 0.7145 to 0.7204, similar to their host rocks (porphyroblastic lava and sub-granodioritic porphyry) which have ε〓 values from -6.2 to -9.4 and I〓 values from 0.7121~0.7192. On diagram of ε〓- t, the fluorites and host rocks plot in similar area within the evolution field of the basement rocks at Xiangshan. The lead isotopic compositions of pyrites formed in uranium mineralization period plot as a line on diagram of 〓Pb/〓Pb vs.〓Pb/〓Pb. The host rocks plot at the lower value end. Calculation based on the slope of the line and the mineralzation age yields age of 144Ma for the geological body which provided uranium for the mineralization.

邹家山和沙洲铀矿床成矿期萤石的ε〓值(-6.7~-8.3)和I〓值(0.7145~0.7204)与赋矿围岩(碎斑熔岩及次花岗闪长斑岩)的ε〓值(-6.2~-9.4)和I〓值(0.7121~0.7192)相似,在ε〓-t图上,成矿期萤石数据点的投影范围与赋矿围岩的基本吻合,且均落在相山元古宙基底演化域范围内;成矿期黄铁矿的铅同位素组成在〓Pb/〓Pb-〓Pb/〓Pb关系图上呈线性分布,而火山岩的铅同位素组成位于此相关线的低值一端;利用异常铅线的斜率及成矿年龄计算出富铀地质体的形成年龄为144Ma,这与赋矿围岩的成岩年龄(135~140Ma)非常接近。

The Holocene deposits were formed during the regression from the early postglacial Tyrrell sea.

全新世沉积时期形成的回归从早期后期泰瑞尔大海。

This paper explains the geological characteristics of the deposits,the technological experimant of producting Potassic magnesium Fertilizer and the prospects of developing utilization.

本文阐述了矿床地质特征、生产钾镁肥的工艺试验及开发利用前景,为相关厂家生产钾镁肥提供了生产依

The mineralization of a number of deposits of this class were associated with certain types of host rocks, but the most were formed by the unmixing of H2O-CO2-salt fluid with very high salinities and the mineralization is commonly linked to potassic alteration.

部分该类矿床的形成与一定的主岩类型有关,而多数矿床可能由高盐度H2O-CO2-盐混合流体的不混溶作用形成,且矿化通常与钾化有关。

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