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动力热液
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  dynamic hydrothermal
     Dynamic Hydrothermal Origin and Prospecting Guides of the Qiandongshan Pb-Zn Depsoit, Fengxian, Shaanxi
     凤县铅硐山铅锌矿床动力热液成因标志与找矿方向
短句来源
     DYNAMIC HYDROTHERMAL ORIGIN OF JINWOZI GOLD DEPOSIT
     金窝子金矿床动力热液成矿雏议
短句来源
     According to the new recognition that Yinshan Cu-Au polymetallic deposit was formed by double-coupling mineralization between tectonic dynamic hydrothermal solution and volcanic-magmatic hydrothermal solution, the system of mineralization zoning of the deposit, sedond-order and multi-centre mineralization zoning model,was set up, and the mechanism and ore prospecting significance were approached.
     根据银山Cu-Au多金属矿床是由构造动力热液和火山-岩浆热液双重耦合成矿作用而形成的新认识,建立了银山矿床新的矿化分带体系──二级多中心矿化分带模式,并探讨了其形成机制及找矿意义。
短句来源
  “动力热液”译为未确定词的双语例句
     A New Type of theGolden Quartz Vein-the Dynamothermal Solution Type
     含金石英脉的新成因类型—动力热液
短句来源
     THE FEATURES OF DyNAMO-HYDROTHERMAL METALLOGENESIS OF THE QIANDONGSHAN LRAD-ZINC DEPOSITS
     铅硐山铅锌矿床动力热液成矿特征
短句来源
     YINSHAN Au-Cu POLYMETALLIC ORE DEPOSIT DOUBLE COUPLING MINERALIZATION OF TECTONO-DYNAMIC AND VOLCANO-MAGMATICHYDROTHERMAL SOLUTION
     江西银山金铜多金属矿床构造动力热液与火山岩浆热液双重藕合成矿作用
短句来源
     GEOLOGICAL AND GEOCHEMICAL CHARACTERISTICS AND TECTONO-DYNAMIC HYDROTHERMAL METALLOGENESIS OF DUSHAN ANTIMONY OREFIELD, GUIZHOU
     贵州独山锑矿田地质地球化学特征和构造动力热液成矿
短句来源
     From the viewpoint and the basic conditions of dynamo-metallogenesis, the geological characters of the deposit are discussed and its forming mechanism is analyzed, and a new suggestion for the mechanism of Dengjiashan Pb-Zn deposit-the stratabound dynamic- hydrothermal Pb-Zn deposit is presented here.
     剪切褶皱和紧闭倒转背斜等和4期构造变形序列. 从动力作用成矿观点和动力矿床形成的基本条件,来认识邓家山铅锌矿床地质特征和分析矿床形成机制,提出了邓家山铅锌矿床为层控型动力热液成因矿床的新认识.
短句来源
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  相似匹配句对
     the power;
     动力论;
短句来源
     Momentum to Civilization
     文明的动力
短句来源
     DYNAMIC HYDROTHERMAL ORIGIN OF JINWOZI GOLD DEPOSIT
     金窝子金矿床动力热液成矿雏议
短句来源
     A New Type of theGolden Quartz Vein-the Dynamothermal Solution Type
     含金石英脉的新成因类型—动力热液
短句来源
     ON HYDROTHERMAL ROCK
     关于热液
短句来源
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The dynamometaliogenesis here means the processes by which ore-hosting beds or source beds have been acted on by certain orented tectonic stresses so that the Ore-forming substances within them are forced to Migrate in different ways and get enriched to form mineral deposits at some suitable tectonic sites.lt is different from the tectonic control during ore precipitation. Based on the geological environments,the conditions under which the ore-forming substances concentrated and the migration ways of these substances,...

The dynamometaliogenesis here means the processes by which ore-hosting beds or source beds have been acted on by certain orented tectonic stresses so that the Ore-forming substances within them are forced to Migrate in different ways and get enriched to form mineral deposits at some suitable tectonic sites.lt is different from the tectonic control during ore precipitation. Based on the geological environments,the conditions under which the ore-forming substances concentrated and the migration ways of these substances, the dynamometallogenesis can be classified into four types, i.e. that of dynamo-viscous flow, of dynamo-differentiation, of dynamo-hydrothermal, and of dy-namo-metasomatic, each having characters for its own in form, tectonic position, and so on.

动力成矿作用系指由定向构造应力作用于含矿层或矿源层而引起矿质以不同方式进行运动和迁移,并在构造有利部位富集成矿的过程。它能直接促使分散的金属元素和化合物活化、迁移、富集而成矿。动力成矿作用分为四种类型:动力粘流作用,动力分异作用,动力热液作用和动力蚀变作用。

On the basis of the study on some stratabound ore deposits and mesothermal and epithermal deposits and in accordance with the theories of thermodynamics, molecular physics and statistical physics, and taking the fundamental principle of minerogenetic types classification into consideration, the author advances a tentative idea concerning "the formation of tectonodynamic hydrothermal solution and metallogenesis" and tries to establish a new mineralization pattern of tectonodynamical origion.

在研究某些层控矿床和中—低温热液矿床的基础上,以热力学、分子物理学和统计物理学的理论为依据,同时考虑到划分矿床成因类型的基本原则,提出了“构造动力热液的成生与成矿”的设想,试图确立一个以构造动力为起因的新成矿模式。

In this article the writer puts forward the concept, the characteristics and the formational mechanism of the dynamo-hydrothermal metallogene-sis. He also classifies the hydrothermal deposits. The dynamo-hydrothermal action is an extremely common metallogenesis.As compared with other hydro- thermal deposits, the ore deposits formed by the dynamohydrothermal activity are of extremely different characteristics,which are remarkably shown in the following aspects:

本文提出动力热液成矿作用的概念、特点、形成机制和热液矿床的新分类。动力热液作用极为常见,它所形成的矿床具有与其他热液矿床极不相同的特点,突出地表现在:成矿物质均系来自围岩,就地成矿;矿脉形态复杂多样、大小不等,且不生根,其分布仅局限于构造破碎带(形变带)之中,同期的矿脉和脉石脉在断裂带的不同构造岩分带中,其形成温度常不相同;不显围岩蚀变。笔者认为,层控矿床主要是通过各种成因的热液对矿源层或贫矿层的改造而成,对矿源层的改造动力热液是起着主要的作用。

 
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