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- In recent years,there more different types Mo deposits(spots) have been discovered in Jilin geosynclinal area,mainly porphyry,quartz vein,skarn and fracture altered rock deposits. 近几年吉林槽区陆续发现多处不同类型的钼矿床(点),其主要类型有斑岩型、石英脉型、矽卡岩型、破碎蚀变岩型。
- Dongchuang Pb Au deposit is a large quartz vein type deposit. 东闯铅、金矿床是一大型石英脉型矿床。
- porphyry type Mo deposit 斑岩型钼矿
- Gold ore main type is auriferous quartz vein type. 金矿床主要为含金硫化物石英脉型。
- Daqingshan gold deposit is a Carboniferous carbonaceous-rock-hosted quartz vein type. 大青山金矿是产于石炭系炭质岩系中的石英脉型金矿。
- The deposit is of filling-metasomatic vein type, genetically belonging to meso-hydrothermal deposit. 矿床成因类型为充填交代型脉状矿床，属中高温热液矿床。
- The gold deposit is of quartz vein type, with the wall rocks consisting of metamorphic rocks of the Jianping Group in age of Late Archean. 金矿体的赋矿围岩为上太古界建平群变质岩系 ,属于石英脉型金矿床。
- Longsheng shear zone type gold deposit is divided into quartz vein type, fine quartz vein type and quartz stockwork type deposit. 桂北龙胜剪切带型金矿划分为石英脉型、石英薄脉型和石英细脉网脉型金矿。
- Banded structures are clue to find quartz vein type gold deposit in this area,and representation of the multi-stage mineralization. 条带状构造是该地区石英脉型金矿的主要找矿标志之一,也是多期次成矿的表现形式。
- Daheishan gold deposit is a fractured alteration type and quartz vein type gold deposit, hosted in the outer contact zone of Damiao granite. 大黑山金矿是赋存于大庙花岗岩体外接触带的破碎蚀变岩型和石英脉型金矿。已发现矿脉8条,以27号脉为主要矿脉。
- Because the composite vein type ore of Jinchangyu gold deposit pre-dates the pink dyke the gold mineralization should occur in late Proterozoic era. 金厂峪金矿床的的复脉型矿化早于肉红色钠长岩脉 ,故其矿化的时代应在晚元古代。
- Wenyu Gold Deposit is a largescale and faultcontrolled auriferous quartz vein type gold deposit in XiaoQinLing gold mineralization belt. 文峪金矿床是小秦岭金矿带内一大型裂控石英脉型矿床，530脉是其主要矿脉之一，其走向近东西，倾向南，倾角中等。
- The Sancha Mo deposit belongs to porphyry molybdenum one,which is a major industry deposit. 三岔钼矿床为斑岩型钼矿床,是该区主要矿床工业类型。
- Hukeng tungsten, located in Wugongshan metallogenic belt in central part of Jiangxi Province, is one large scale quartz vein type wolframite deposit. 浒坑钨矿床是位于江西省中部武功山成矿带的大型石英脉型黑钨矿床。
- It also demonstrates that when closing and reclosing overvoltages are only limited by different type MO As, terminal switching overvoltage of each line is be. 在主送电源线路发生瞬时性故障时,依靠故障解列装置动作跳开接入终端变电所的小电源开关,以满足大系统侧检无压重合闸的需要。
- Gangjiang porphyry Cu, Mo deposit occurs in the spotted medium-grain amphibole-biotite monzonitic granite and is controlled by fault arid joints and fractures near the fault. 摘要岗讲斑岩型铜钼矿产于续迈单元含斑中粒角闪黑云二长花岗岩中，受断层带及附近节理、裂隙的控制，矿区有弱硅化、钾化、黄铁矿化、青磐岩化、泥化等蚀变；岗讲现已圈定矿体4个。
- Zhuangzi Au deposit is located at the contact zone between Guojialing granitic body and Ci shan granitic body and Jiaodong group and is dominated by quartz vein type Au ore. 山东栖霞庄子金矿床产于郭家岭花岗岩和磁山花岗岩与胶东群的接触带,矿石以石英脉型为主,金品位高且发育明金。
- Gangjiang porphyry Cu,Mo deposit occurs in the spotted medium-grain amphibole-biotite monzonitic granite and is controlled by fault and joints and fractures near the fault. 岗讲斑岩型铜钼矿产于续迈单元含斑中粒角闪黑云二长花岗岩中,受断层带及附近节理、裂隙的控制,矿区有弱硅化、钾化、黄铁矿化、青磐岩化、泥化等蚀变;
- K-Ar ages of granitoids in Sanya, Baishiquan and Hongliugou area (Qin et al., 2006;Xu, 2007, PhD Thesis) and Molybdenite Re-Os age of Baishan Mo deposit (Zhang et al. 且由于含矿火山岩含有花岗岩的角砾，表明其形成明显晚于上述花岗岩，即与成矿密切相关的火山-次火山岩晚于晚三叠纪，为中生代的产物（秦克章等，2006；
- The Jinduicheng porphyry Mo deposit was formed during the transforming stage of the Qinling Orogen from compression to extension in Mesozoic_Cenozoic period. 钼矿床的成矿物质主要来自钾长斑岩，围岩不提供成矿物质。
