The two types involve orogenic belt gold deposit and epithermal gold deposit.
根据金矿床在成矿作用、主要控矿因素、矿石建造和组构、容矿岩石建造等方面的特征划分为2种金矿类型:造山带型金矿床和浅成低温热液金矿床。
New advances on epithermal gold deposits;
浅成低温热液金矿床研究进展
Latest advances of researches on epithermal gold deposits
浅成低温热液型金矿床若干问题的最新研究进展
This paper documents epithermal deposits in the northeast China and proposes a geological map showing their spatial distribution.
通过中国东北地区浅成低温热液矿床的综合特征研究,将矿床的分布划分为德尔布干、呼玛、小兴安岭和吉东4个矿集区,根据其矿床地质、地球化学特征初步确定成矿流体主要来自大气降水,部分混有岩浆水;成矿物质主要来自赋矿围岩和成矿岩浆-流体系统;多数矿床形成于中低温、中浅成环境,个别矿床成矿温度高、深度大,显示了斑岩型或造山型与浅成低温溶液型成矿系统之间的连续性;厘定大规模成岩成矿时间为130Ma左右,构造环境是古亚洲洋闭合后陆陆碰撞过程的挤压-伸展转变体制,并以矿集区尺度的CMF模式解释了浅成低温热液矿床岩浆-流体系统的发育机制。
A series of epithermal deposits and mineralized occurrences including g old,silver,copper,lead,and zinc resources were discovered in the Mesozoic volcanic-subvolcanic rocks i n Manzhouli area.
满洲里中生代火山-次火山岩发育区,发现了一系列浅成低温热液矿床,矿种有Au、Ag、Cu、Pb、Zn等。
The tectonic backgrounds of epithermal deposits are mainly island arc and arc-back extension belt.
浅成低温热液矿床形成的构造环境主要为岛弧和岛弧之后的张裂带 ,大多数形成于第三纪 ,少数矿床形成于中生代和古生代 。
Discovery of epithermal Au-Sb deposits in Gangdese metallogenic belt of Tibet and its significance: Case study of Longruri Au-Sb deposit;
西藏冈底斯成矿带浅成低温热液型金锑矿床的发现及其意义——以西藏弄如日金锑矿床为例
epithermal gold deposit
浅成低温热液金矿床
The Ore- forming Fluid and Mineralization of Epithermal Gold Deposits in Pinyi, Western Shangdong;
鲁西平邑地区浅成低温热液金矿床成矿流体及成矿作用
Wang L J,Wang JB,Wang YW,Zhu HP and Qu LL.2005.The study of ore-fluid and C-S-Pb isopope of rich in S and poor in S types in epithermal gold deposits,Junggar area,Xinjiang.
新疆准噶尔地区富硫型与贫硫型浅成低温热液金矿床成矿流体与碳、硫、铅同位素
Mineralization zoning of epithermal Au-Ag polymetallic deposit and its prospecting criteria
浅成低温热液金银多金属矿床矿化分带及找矿标志
Metallogenic Characteristics and Searching Prospect of Epithermal Gold Deposits in Xiangnan;
湘南浅成低温热液型金矿成矿特征及找矿前景
Latest advances of researches on epithermal gold deposits
浅成低温热液型金矿床若干问题的最新研究进展
Mineralization enrichment of uranyl mineral in mid-low temperature hydrothermal of Shuanghuajiang uranium deposit
双滑江铀矿床低温热液铀酰矿物富集成矿作用
Study on the Metallogenesis and Models in Mesozoic Epithermal Gold Deposits in Yanbian, Jilin Province;
延边中生代浅成热液铜金矿床的成矿模式研究
Metallogenic Model of Epithermal and Low-sulfidation Gold Deposit, Yanbian Area
延边地区浅成低温低硫化型金矿床的成矿模式研究
Tertiary-type ore deposit
(浅成热液矿床) 第三纪型矿床
HUOSHANCUN MIDDLE-LOW T HYDROTHERMAL PB-ZN MULTIMETALLIC DEPOSIT IN WEISHAN
巍山火山村地区中低温热液型铅锌多金属矿
Gold deposition mechanism is the key to understanding the mineralization mechanism of hydrothermal deposits.
金的沉淀机理是了解热液金矿床成矿机制的关键。
REGIONAL METALLOGENIC RULE OF VOLCANIC-SUBVOLCANIC HYDROTHERMAL METAL ORE DEPOSITS, MESOZOIC, JILIN
吉林省中生代火山—次火山热液金属矿床的区域成矿规律
The genesis of the deposit belongs to hydrothermal-exhalation stratabound deposit of syngenetic fault.
矿床成因属于同生断裂喷流热液层控矿床。
On Discremination of Postore Dykes in Early Precambrian Hydrothermal Deposits
早前寒武纪热液矿床成矿后岩脉的鉴别
MULTI-FIELD STACKING METHOD FOR LARGE-SCALE HYDROTHERMAL ORE DEPOSITS PREDICTION
热液矿床大比例尺成矿预测的多场叠合法
The Preparation of Rutile TiO_2 Nanosphere in Liquid Phase at Low Temperature;
低温液相合成金红石型TiO_2纳米球
In all hydrothermal deposits the minerals formed are not solely the sulfide ore minerals.
在所有热液矿床中，所形成的矿物并不单单是硫化物矿石矿物。
