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mineralizing相关的网络例句

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The Jinshan gold deposit suffered superposed reconstruct by hydrothermal mineralizing process in the Palaeozoic era.

金山金矿床在形成过程中还经历了古生代热水成矿作用的叠加改造。

Mineralizing fluid migrated, concentrated and allocated in the fractured zone between granite and metamorphic rock, it was a good canal for Rn, U, Tb and K, added intense sericitization, in geophysical exploration we found that y -ray spectrometry, Radon spectrometry can reflect the allocation of fractured zone, X-ray fluorescence analysis in laboratory can effectively find alteration envelope, elements geochemical abnormality, soil primary and secondary halo, then find deposits allocation.

结合矿床特征,以核技术为主的找矿方法中γ能谱及氡测量能很好地反映容矿破碎带及花岗岩与变质岩的接触位置,室内多元素X射线荧光测量技术可以有效寻找蚀变带、元素地球化学异常及土壤原生晕、次生晕等流体成矿地球化学界面的标志,快速追踪矿床的位置。

The gold mineralization belt, mineralizing type and form of gold deposits were controlled by this ductile shear zone.

该剪切带对该区的金矿化异常带、矿化类型乃至矿床的形态和产状具有严格的控制作用,指出了韧性剪切带型应为本区金矿的主要类型。

On the other hand, this text Will use the similar dimension of fractal theory to the data of distribution of the mineralizing element,ore, structure to set up unusual lower limit of them and has probed into the

另一方面将分形理论中的相似维数算法运用于金元素分布数据,矿点数据,图文资料当中,从而建立金元素分布的异常下限、线性构造分布的异常下限以及金矿点分布的异常下限,并且进一步对结果从定量的角度探讨了三者的关系。

Thus, the hydrogeochemistry of mineralizing condition and prediction of North-Western sandstone type uranium ore in Chine Have all round been known by us.

并由此对我国西北砂岩型铀矿成矿条件和成矿预测中的水文地球化学有了一个较全面系统的认识。

Which were found in succession in the Yili Late Paleozoic volcanic rock province in the north section of West Tianshan Mountains ,are considered as epithermal mineralizing type,and furtherly divided into adular sericite sub type and silicated rock sub type.

20世纪90年代,在新疆西天山北段晚古生代火山岩区内相继发现了阿希大型金矿床及其外围的伊尔曼得、恰布坎卓它等金矿床,并进一步确定了其系产于晚古生代火山岩内的浅成低温矿床。

After thermodynamic studies on the former two typical fine disseminated gold deposits, the following facts are found: both existent and transferring form of gold in mineralizing hydrothermal solution are predominated by Au 〓 and AuH〓SiO〓; the contribution of AuCl〓〓 is negligible to mineralization; and those contribution of gold bearing complexes including Au with As-S and Sb-S are much less than that of Au 〓 and AuH〓SiO〓, organic complex take effect in some degree during the relatively low temperature activating period of gold.

对以上两个典型微细浸染型金矿床的热力学研究,发现成矿热液中金的存在和迁移形式均以Au〓和AuH〓SiO〓为主,AuCl〓对金迁移成矿的贡献微不足道,金砷硫或金锑硫等复合配合物对金成矿的作用远不及Au〓和AuH〓SiO〓,有机配合物在温度较低的金的活化期有一定作用。

In the North Ordos basin the sandstone-type uranium deposits developing in the system of sandstone beds of sedimentary facies of braided river course in Midde Jurassic Series,at the same time it happen some show of ore:the alteration zone of chloritization,bleaching decoloration and carbouation of epigenetic alteration,which show of ore are immediate and indirect for uranium mineralizing process.

摘 要:发育于内蒙古鄂尔多斯盆地北部中侏罗统直罗组辫状河相杂砂岩体内的砂岩型铀矿,有一系列较为特殊的与放射性铀成矿有直接或间接关系的成矿地质现象:绿色化蚀变带、漂白退色化带、二次胶结钙化砂岩团块及钙化砂岩断续层与&钙化木&后生蚀变现象;在与铀矿化和与油气的关系认识上存在一定分歧。

Results showed that in the water body of Xizi Lake, annual average of culturable planktonic ammonifiers and nitrogen fixers were 510 and 236 CFU/mL, respectively; Ammonia oxidizers, nitrite oxidizers, nitrate reducers and denitrifiers were 8.5, 16, 587 and 16 MPN/mL, respectively; Inorganic phosphate solubilizing bacteria (1PB) and organic phosphorus mineralizing bacteria were 89 CFU/mL and 37 MPN/mL, aerobic and anaerobic cellulose decomposers were 7 and 5 MPN/mL, respectively.

水体中可培养异养细菌和固氮菌的年平均值分别为510和236CFU/mL,氨氧化细菌、亚硝酸氧化细菌、硝酸盐还原菌和脱氮菌的数量分别为8.5、16、587和16 MPN/mL;无机磷和有机磷分解菌分别为89 CFU/mL和37 MPN/mL;好氧性纤维素分解菌和厌氧性纤维素分解菌只有7和5 MPN/mL。

By the introduction of geotectonics,mineralized geological background and characters of several epithermal gold deposits in Southeast Asia,the ore-forming circumstance and its causes of changes,mineralizing materials' sources and the main reasons for gold deposition in different conditions was discussed.

文章介绍了东南亚地区几个浅成低温热液金矿床的成矿地质背景、矿床地质特征,分析了矿床形成环境及变化的原因、成矿物质来源和导致金在不同环境下沉淀的主要因素,并讨论了浅成低温热液矿床形成的几个问题。

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