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   地下水成矿作用 的翻译结果: 查询用时:0.162秒
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地下水成矿作用
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  “地下水成矿作用”译为未确定词的双语例句
     Some current achievements of researches into deep groundwater are obtained in determining basic genetic types of groundwaters, establishing series of effective methods for paleohydrogeological analysis of ore forming processes, and developing some computer programs of geochemical modeling of water rock interactions.
     近年来,国内外有关深部地下水研究的主要成果有:阐明了地下水的基本成因类型; 建立了地下水成矿作用研究中的一套古水文地质分析方法;
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  相似匹配句对
     ORIGIN OF DEEP GROUNDWATER AND ITS ORE FORMING PROCESSES
     深部地下水的起源及其成矿作用
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     Eliminating iron ion in groundwater
     地下水除铁
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     10. Underground water;
     10.地下水;
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     Metallogeny in Relation to Supercontinent
     超大陆旋回和成矿作用
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     5. regional mineralization;
     5.成矿作用的区域性;
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Some current achievements of researches into deep groundwater are obtained in determining basic genetic types of groundwaters, establishing series of effective methods for paleohydrogeological analysis of ore forming processes, and developing some computer programs of geochemical modeling of water rock interactions. This paper introduces how to determine the origin of groundwater by using the isotopic data of groundwater and gas. Paleohydrogeological analysis of ore forming processes and chemical features and...

Some current achievements of researches into deep groundwater are obtained in determining basic genetic types of groundwaters, establishing series of effective methods for paleohydrogeological analysis of ore forming processes, and developing some computer programs of geochemical modeling of water rock interactions. This paper introduces how to determine the origin of groundwater by using the isotopic data of groundwater and gas. Paleohydrogeological analysis of ore forming processes and chemical features and origins of sedimentary basinal waters are also illustrated.

近年来,国内外有关深部地下水研究的主要成果有:阐明了地下水的基本成因类型;建立了地下水成矿作用研究中的一套古水文地质分析方法;开发了一系列用于水—岩相互作用研究的地球化学模拟软件。文章重点介绍了如何利用地下水及其气体的同位素资料来判别地下水的成因,同时亦说明了成矿作用的古水文地质分析、沉积盆地水的化学特征及其成因,以及沉积盆地水的成矿作用方面的研究成果与方法。

Lanping basin lies between Lancangjiang fault and Jinshajiang fault. Himalayan movement is the important tectonic event, during which the act ivity of mid-alkali magma is strong. Previous work focused on studying porphyry copper, lead, zinc polymetallic ore deposits in this area and ignored the rel ationship between Himalayan tectonomagmatic movement and polymetallic mineraliza tion in the basin. The tectonomagmatic movement occurred at the same time as lea d zinc polymetallic mineralization, that is, Himalayan...

Lanping basin lies between Lancangjiang fault and Jinshajiang fault. Himalayan movement is the important tectonic event, during which the act ivity of mid-alkali magma is strong. Previous work focused on studying porphyry copper, lead, zinc polymetallic ore deposits in this area and ignored the rel ationship between Himalayan tectonomagmatic movement and polymetallic mineraliza tion in the basin. The tectonomagmatic movement occurred at the same time as lea d zinc polymetallic mineralization, that is, Himalayan period. Magma activity an d mineralization is controlled by the same faults in Lanping basin and its adjac ent area. Magmatic rocks and ore rocks have similar pattern of REE, and have high contents of Th, Cr, Co, Ni. These characteristics of elemental geochemistr y reveal the basic relationship between magmatic movement and mineralization.

以往人们对兰坪盆地铅锌多金属矿床成因的研究 ,大多侧重于对古地下水成矿作用和热水沉积改造作用探索 ,而忽视了盆地内构造 -岩浆活动对该区多金属成矿作用的贡献。本文重点研究了兰坪盆地及邻区喜山期岩浆岩的微量元素地球化学特征 ,并对岩浆活动与流体成矿的关系进行了详细的讨论

 
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