成因类型属次火山岩型中温热液银多金属矿床。
Silver polymetallic deposits at Dongwushan is genetically related to the subvol canic type of moderate temperature thermal deposits.
呷村含金富银多金属矿床属海相火山喷流-沉积矿床。
Gacun argentiferous polymetallic ore deposit is a volcanic exhalation - sedimentary deposit.
二郎坪群蛇绿岩中多金属矿床属火山成因块状硫化物矿床。
The poly metallic deposit occurred in the Erlangping ophiolite of eastern Qinling Mountain was regarded as volcanogenic type.
贵州银厂坡银矿床属银铅锌多金属矿床，其规模近于中型。
Yingchangpo silver deposit of Guizhou is an Ag_Pb_Zn polymetallic deposit that approaches middle scale.
在成矿机制上与金顶铅锌矿床相似，属以热卤水成矿为主的多成因的层状多金属矿床。
It is similar to the Jinding Pb-Zn deposit in metallogenetic mechanism, belonging to the polygenetic bedded polymetallic deposit with hot brine as the principal metallogenetic factor.
该矿是发现最早的破碎带蚀变岩型金矿床，其成因属重熔岩浆中温热液型。
The mine is the earliest discovered broken belt altered rock type gold deposit, it belongs to remelting magma mesothermal type.
安徽庐江龙桥铁矿属一大型隐伏磁铁矿矿床。
The Longqiao iron ore deposit is a large-scale hidden magnetite ore deposit.
秦岭泥盆系铅锌成矿带中闪锌矿微量元素特征表明矿床属海底喷气成矿，成矿流体温度为低温。
The microelement signature of the sphalerite in the Qinling Devonian system Lead-zinc metallogenic beltindicates that the deposits belong to submarine exhalation-sedimentary.
桃园钼矿床属中温热液脉型矿床，围岩蚀变具线型对称特征。
Taoyuan molybdenum ore belongs to mesothermal hydrothermal vein deposit. Alteration of country rock has linear feature.
矿床属陆相砂砾岩型铜矿。
The mineralization type is continental sandstone (conglomerate) copper deposit.
狮子山铜矿是长江中下游大型埋藏型铜矿之一，属矽卡岩型伴生金银铜矿床。
Shizishan Copper Mine is a skarn deposit living with gold and ciliver, one of the big buried Copper Mines in the downstream of Yangtze River.
研究发现中国某些优质锰矿，属复成矿床，它们都是地洼成矿作用的产物。
Some high quality manganese ore deposits of China are found to be polygenetic compound ore deposits which are the products of diwa mineralization.
蒲塘金矿床属爆破角砾岩型。
毒重石矿床属热水沉积成因层控矿床。
Witherite deposits belong to stratabound deposits of hot water sedimentation.
录斗艘金矿床属破碎蚀变岩型金矿，产于德乌鲁石英闪长岩与录斗艘石英闪长斑岩接触带附近。
Ludousou gold deposits belong to fractured altered rock-type gold deposit, produced in Dewulu quartz diorite and Ludousou quartz porphyry contact zone.
汤家坪钼矿属典型的斑岩型钼矿床。
Tangjiaping molybdenum is a typical porphyry type molybdenum deposit.
蔷薇辉石矿床的形成主要经历了沉积期和区域变质期两大阶段。成因类型属变质岩型低温变质相蔷薇辉石矿床。
The rhodonite deposit was for- med mainly through two stages, sedimentation and regional metamorphism, and its genetic type belongs to epithermal metamorphic facies.
拱丁金矿床属石英脉型。
初步认为该矿床属层控型金矿床。
It is considered that the gold deposit belongs to stratabound deposit.
矿床形成与柴北缘区域地壳多阶段演化和多次成矿作用有关，属多因复成矿床。
The deposit belongs to a poly genetic compound gold deposite resulting from multi mineralizations and its formation is associated with multi stages evolution of the crust in the area.
鞍山小岭子铁矿系沉积变质矿床，铁矿物嵌布粒度细，磁性率低，属较难选铁矿。
Anshan Xiaolingzi iron ore belongs to the sedimentary metamorphic iron deposits with characteristics of fine iron minerals and low magnetic rate, and it is a refractory iron ore.
本文通过成矿地质背景和成矿规律分析，认为黔西北地区铅锌矿属沉积改造型铅锌矿床。
In this paper, by analyses the metallogenic regulation and metallogenic geologic background, it thought the lead-zinc deposit in northwest Guizhou belong to depositing-reworking lead-zinc deposit.
正在勘探中的新疆哈巴河县阿舍勒铜锌矿床，属海相火山喷气-沉积成因。
The Ashele copper zinc deposit that is under exploration in Habahe County, Xinjiang, is of Marine volcanic exhalation-sedimentary origin.
此矿床之矿石属钙基膨润土，经适当选矿后可用于深加工。
After proper ore dressing, the ores can be used for deep procession.
大坪金矿床属石英脉型多金属硫化物矿床。
The Daping gold deposit belongs to a polymetallic deposit of gold-sulfide quartz vein type.
矿床成因属第四纪残积型。
The origin of the deposit belongs to Quarternary eluvial placer type.
吉家洼金矿床矿石属少硫化物型金矿石，矿物种类丰富，金属矿物含量约5 %，脉石矿物含量约95 %。
The ores of Jijiawa gold deposit are ores with low content of sulfide. The minerals are rich in the ores. The contents of mineral and rocky mineral are about 5% and 95% respectively.
矿床成因属风化残积型，受地层、岩性的控制。
Genetically, it is an eluvial deposit produced by weathering, controlled by the stratigraphy and lithology.
矿床成因属风化残积型，受地层、岩性的控制。
Genetically, it is an eluvial deposit produced by weathering, controlled by the stratigraphy and lithology.
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