1) metallogenic maps
成矿图
2) metallogenic map
成矿图
3) mineralization
成矿
1.
Geochemical characteristics and mineralization of the Cretaceous period magmatic rock of the Bailiping silver-polymetaltic ore-concentrated province,Helong area;
和龙百里坪银、多金属矿化集中区白垩纪岩浆岩地球化学特征与成矿
2.
The tectonic evolution and mineralization of Zheboshan gold deposit in northwest Sichuan;
川西北哲波山金矿床构造演化与成矿
3.
A comparison of Yanshanian granitoids between the Zhejiang-Jiangxi-Anhui border area and the Dexing and Tongling mineralization-concentated areas, with a discussion on mineralization;
浙赣皖相邻区与德兴、铜陵矿集区燕山期花岗岩类岩石对比研究及其成矿
4) ore-forming
成矿
1.
Relationship between granite porphyry and ore-forming in Liaoning Wulong gold area;
辽宁五龙金矿区花岗斑岩与成矿关系浅析
2.
By the study on ancient stress,fluid inclusions and composition of tectonites andstructural ores from gold deposits,the ore-forming mechanism of critical transition in ore-bearing ductile-brittle fractures is analyzed, involving the metallogenic dynamics,fluid evolution and the structural mechanism during the evolving process of fractures from ductile to brittle natures.
通过对金矿构造岩、构造矿石的古应力、流体包裹体和物质成分等的研究,探讨了断裂构造从韧性到脆韧性的演化过程中,界面转换成矿的特征,包括动力学特征、流体演化特征、构造对流体的驱动机制等。
5) metallogenic series
成矿系列
1.
Characteristics of typical iron ore deposits and their metallogenic series in Qinghai Province;
青海省典型铁矿矿床特征及其成矿系列的浅析
2.
Based on the analysis of deposit genetic type in the metallogenic belt,the metallogenic series has been put forward,that is volcanic-subvolcanic hydrothermal and porphyry type Au-Cu and Mo-Pb-Zn-Ag metallogenic series.
在分析成矿带内不同矿床成因类型的基础上,建立了该成矿带的成矿系列:火山、次火山热液-斑岩型金铜及钼铅锌银成矿系列。
3.
According to mineralizing characters of the different terranes,five nonferrous metals metallogenic series are concluded.
文章从地体的形成与拼贴方面讨论了湖南省5个构造地层地体的划分,根据各地体的成矿特征不同,按元素组合归纳出五大有色多金属成矿系列,引用“液态矿源层”概念解释大型、超大型矿床的巨量物质来源,认为地体边界断裂带和地体内深大断裂控制了有色金属大型、超大型矿床与矿集区的分布。
6) metallogenic prognosis
成矿预测
1.
Location-vacancy of metallogenic series and its application to metallogenic prognosis;
成矿系列的缺位问题及其在成矿预测中的应用
2.
Application of GIS to metallogenic prognosis: Case study of Yangjiazhangzi ore field;
GIS技术在成矿预测中的应用实例——以杨家杖子矿田为例
3.
Application of variable structure neural net model in metallogenic prognosis;
变结构人工神经网络模型及其在成矿预测中的应用
7) mineralization
成矿作用
1.
Epithermal mineralization in the Western margin of the Luzon arc:Lalab gold deposit;
吕宋岛弧西缘浅成低温热液成矿作用—以拉拉布金矿床为例
2.
Initial discussion on geological characteristics of the Erbahuo silver deposit of Wengniute Inner Mongolia and its mineralization;
内蒙古翁牛特旗二把伙银矿地质特征及成矿作用初探
3.
Hydrothermal mineralization of Au (Ag)-polymetallic ore deposit in the volcanic rock series of the Xiong'er Group;
熊耳群火山岩系金银多金属矿床热水成矿作用
8) metallogenesis
成矿作用
1.
Geological characteristics and metallogenesis of Sawayaerdun gold deposit in southwest Tianshan Mountains, Xinjiang;
新疆西南天山萨瓦亚尔顿金矿床地质特征及成矿作用
2.
The possible connection of the earth electric force and magnetic force controlling metallogenesis;
地球电、磁力对成矿作用控制的可能联系
3.
Post-orogenic dike complexes and implications for metallogenesis;
造山后脉岩组合与内生成矿作用
9) mineralization mechanism
成矿机制
1.
Based on the analyses of mineral components,structure,structural characteristic,ore layer,the wall rock alteration and depositionai environment in different ore field,this paper further discusses origin and the mineralization mechanism of the Hongshan iron ore deposit.
红山铁矿赋存于青白口系大豁落山群第四岩组第二岩性段,属于热卤水喷流沉积铁矿床,本文通过对不同矿区矿床矿石的矿物组分、结构、构造特征,矿层及围岩蚀变与沉积环境分析,进一步探讨了红山铁矿床成因及成矿机制。
10) metallogenic regularity
成矿规律
1.
Discovery of cryptoexplosive breccia in Nanjinshan gold deposit of Beishan area,Gansu Province and study of metallogenic regularity;
甘肃北山地区南金山金矿床隐爆角砾岩体的发现及成矿规律研究
2.
Exploration on metallogenic regularity of gold-antimony deposit in Mazhala,south Tibet;
西藏南部马扎拉金锑矿成矿规律初探
3.
Geological characteristics and metallogenic regularity of underground brine ore in coastal areas of Weifang,Shandong Province;
山东潍坊沿海地下卤水矿地质特征及成矿规律
补充资料:成矿分带
成矿分带 metallogenic zone 在含矿流体的活动过程中,由于地质因素和物理化学条件的变化,导致不同的矿石依次产出,形成不同矿石组合的带状分布。例如,在沉积铁矿床中,常表现出不同的矿石相沿沉积当时的海岸作带状分布,距岸由近到远的成矿分带为:①氧化物带(赤铁矿);②硅酸盐带(鲕绿泥石);③碳酸盐带(菱铁矿);④硫化物带(黄铁矿)。又如在气化热液矿床中,含矿气液随着离热源距离的增大,以及物理化学条件的变化,不同矿物的沉淀常依次成带状。例如,中国湖南柿竹园矿床中,自含矿花岗岩体向外,或由深处向浅处,可分出钨带→锡带→铋带→铜带→锌带→铅带。 成矿分带按其空间产出情况,有水平分带和垂直分带;按其规模大小,有区域成矿分带、矿床分带和矿体分带。区域成矿分带受多种因素控制,如中国江西南部为钨矿带,北部为铜(金)矿带,这是因为两地的构造背景、岩浆岩类型及变质岩基底等有明显差异造成的。 成矿分带反映了成矿作用在空间上的变化规律,查明这种带状分布规律,对指导矿产勘查和矿山开发均有实际意义。 |
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条