成矿系统是当今矿床学研究的一个新领域。
The ore forming system is a new domain in the study of geology of ore deposits.
这一成矿系统是同一能量场和流体场、不同矿源场之间耦合的结果。
The metallogenic system is the couple results of the same energy field, fluid field and different ore source field, and has good potential for ore prospecting.
最后，用“三环图”表示了地球系统、成矿系统和勘查系统的辩证关系。
Finally, the paper USES a "figure with 3-rings" to express the dialectical relationship among the Earth system, metallogenic system and exploration system.
成矿系统的研究方向为：（1）继续开展成矿系统理论和分析方法的研究；
The main research fields of the ore forming system have been summarized follow: (1) continue to study the theory and analysis method of the ore forming system;
在这种背景下，产生了“综合成矿论”和“成矿系统论”，两者有许多异同之处。
Under this background, comprehensive metallogenic theory and the metallogenic system theory come up, which have many differences and similarities.
流体成矿系统内具有一些重要特征，如各种地质要素的方向性、相关性和指示性变化。
There are several major characters such as the directive, relative and indicative changes of various geological features within a fluid ore forming system.
预测理论有相似类比理论、矿床模型理论以及地质异常理论、成矿系列和成矿系统理论等。
The predication theories include of similar analogy, ore deposit model, geo-anomaly, deposit metallogenic series and metallogenic system.
以构造动力成矿系统理论为基础，通过构造成因及演化过程说明海西-燕山期是充水裂隙形成的重要阶段；
The structural information and evolution of the fissured-water pour-in on the basis of theory about Zhaoping structure mineralized dynamic system are analyzed.
文章分别阐述了矿床的和区域的构造—流体—成矿系统，结合矿床和区域实例讨论了它们的研究目的、内容和方法。
This paper discusses predominantly the aim, content and approaches of the study on regional and orefield scales of structure fluid ore forming processes respectively.
然后进一步将其具体化为三大组成部分，即（1）矿床的动力学属性，（2 ）矿床地质学场，（3 ）成矿系统的演化。
Then it is realized and specified by three major constituent parts, i. e. (1)dynamical attributes of ore deposits, (2)fields of ore geology and (3) evolution of ore-forming systems.
逆冲推覆构造系统沿八家子盆地东缘和北西缘分布，控制铅锌矿床的就位与分布，为成矿期构造。
Thrust nappe system, extending along southeast and northwest margin of Bajiazi basin. controls the emplacement and distribution of Pb-Zn deposits, so it is metallogenic structure.
对沽源-多伦盆地火山岩类和花岗岩类进行了同位素地质年代学、地球化学和铀成矿条件的系统研究。
The results of systematic studies of geochronology, geochemistry and uranium metallogenic condition of volcanic rocks and granites in Guyuan-Duolun Basin are reported.
该系统包括“三大”成矿体系，即：幔源岩浆体系、深穿透断裂构造体系、含矿气液流体体系。
The mineralization system has three giant system, namely mantle magmatic system, penetrability deep-fault and ore- bearing pneumato-hydrothermal system.
化探数据系统分析可以提取与不同成矿单元尺度水平相应的信息，其中包括矿床主控因素的信息。
The system analysis of geochemical data can help information in accordance with the scale level of different mineral units including main ore-controlling factors.
由导矿构造、储矿构造和成矿构造流体等子系统组成了成矿构造的功能结构。
The ore-forming function structure is composed of subsystems including mineral transfer, mineral deposition and ore-forming tectonic fluid.
开发的系统初步实现了专家系统与GIS的结合，可以在区域成矿远景区划和评价中应用。
Combining the export system with GIS, the digital mineral resource assessment system can be applied to the prospective assessment of mineral deposits and regional planning.
对产在五朵山花岗岩中的矿床（点）的地质背景、矿床特征、成矿流体及矿床成因等方面作了系统的研究。
The geological setting, deposit features, metallogenetic fluid and the genesis of the gold deposit hosted in the Wuduoshan granite were systematically discussed.
阿舍勒矿床自发现以来对其成矿规律的研究一直未系统地分析和总结过，本文即是对其成矿规律的一个初步探索。
The metallogenic rule in Ashele deposit has never been analyzed and summarized since the deposit was found, and this paper is an exploration in the rule.
区内成矿流体系统可分为紫金山子系统与公郎弧子系统。
The ore-forming fluid system in Weishan-Yongping ore concentration area can be divided into two subsystems, namely, Zijinshan subsystem and Gonglang arc subsystem.
矿产系统勘查是把系统论的思想同矿产勘查过程紧密结合形成矿产系统勘查体系。
Systematical exploration system for mineral resources is formed by combining the systematical theory with exploration process for mineral resources.
在此基础上，建立了区域中生代构造-流体-成岩成矿地球化学-体化系统模型。
The Mesozoic magmatism and polymetallic mineralization was caused by interaction between deep-derived fluids and Mesozoic multistage tectonic activities.
通过该评价系统共圈出12个成矿预测区。
Through these two evaluation systems, 12 ore-forming predication areas are circled, .
但对本区构造-岩浆-成矿的耦合关系缺乏系统认识。
Whereas there was not system cognition in coupling connection of tectonic-magma-mineralization.
软流圈减压熔融流体系统提供了岩浆侵位动力和成矿物质来源。
The decompression melting fluid system of asthenosphere provides the driving force for magma emplacement and metallogenic material.
系统研究了毛堂、蒲塘金矿床的地质地球化学特征，探讨了金矿化成矿机理。
Geological and geochemical characteristics of the Maotang and Putang gold deposits are described, and the metallogenic mechanism of the gold deposits studied.
成矿流体主要来源于次斜长花岗斑岩携带的热流体，其次是断裂系统的冷流体。
Ore forming fluid was composed of mainly the thermal fluid supplied bY the subplagio granite porphyry and subordinately the cool fluid come from the fracture structure.
从构造演化—岩浆作用—成矿流体系统将火山岩-花岗岩型铀矿作为统一体开展成矿作用研究。
Uranium deposits of both volcanic and granite type are studied as the systematic process of tectonic evolution-magmatism-metallogenic fluid action in South China.
据深部资料结合区域地质特征分析，矿床为一滑覆构造系统。该系统上、下均有砂泥岩作屏蔽层，中间为云岩，形成一个对成矿极为有利的构造封闭系统。
According to regional geology and deep data, the deposit is considered as a gliding nappe system, whose upper and lower shielding layers are sandy mudstone, the middle part is dolomite.
我国南方地洼盆地构造演化、流体演化和砂岩铜矿成矿作用三者之间具有密切的关系，处于一个统一的系统之中。
There is a close relation among tectonic evolution, fluid evolution and formation of sandstonecopper deposits in diwa basins of South China.
我国南方地洼盆地构造演化、流体演化和砂岩铜矿成矿作用三者之间具有密切的关系，处于一个统一的系统之中。
There is a close relation among tectonic evolution, fluid evolution and formation of sandstonecopper deposits in diwa basins of South China.
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