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- 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。
- 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;
- 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。
- Similar to the other orebodies lying along the northwest tectonic belt, the Xiongcun orebody is a porphyry Cu (Au) deposit consisting of a hornblende quartz diorite complex. 雄村铜(金)矿与矿区北西向构造带上多处矿体的特征相似,为一由角闪石石英闪长玢岩杂岩体侵入而形成的斑岩型铜(金)矿床。
- Strong alteration-mineralization occur around the Zijinshan volcanic edifice, forming high-sulfur epithermal Cu-Au deposits, low-sulfur epithermal Ag-Au deposits and porphyry Cu (Mo) deposits. 围绕着紫金山火山机构发育强烈的蚀变矿化,形成高硫型浅成低温热液铜金矿、低硫型浅成低温热液银金矿和斑岩型铜(钼)矿床。
- 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。
- DETERMINATION OF ORE- AND ROCK- FORMING TIME OF THE MACHANGQING PORPHYRY Cu(Mo) DEPOSIT, WESTERN YUNNAN PROVINCE 滇西马厂箐斑岩铜(钼)矿床成岩成矿时限的厘定
- porphyry Cu polymetallic deposit 斑岩型铜多金属矿床
- Most porphyry Cu deposits in the world occur in magmatic arc settings and are formed in association with calc-alkaline arc magmas related to subduction of oceanic-slab. 摘要世界范围内大型-巨型斑岩铜矿多数产于岩浆弧(岛弧、陆缘弧)环境,含矿斑岩岩浆起源与大洋板块的俯冲作用有关。
- 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。
- It is suggested that the eastern Tianshan has great potential for Cu, Ni and Mo deposits and 28 areas have been selected as target for further exploration. 通过研究认为,东天山地区尤以铜、镍、钼矿产资源潜力很大,优选出28个矿找矿靶区。
- porphyry Cu (Mo) deposit 斑岩铜(钼)矿
- 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;
- Keywords Porphyry Mo deposit;wallrock alteration;Tangjiaping; 斑岩钼矿;围岩蚀变;汤家坪;
- Qulong porphyry Cu-Mo deposit 驱龙斑岩铜钼矿床
- Keywords Calc-Alkalic;Alkalic Rock Series;Lithological Character;Volcanic Eruption;Porphyry Cu Deposit;Secondary Enrichment;Minle Jinggu; 关键词钙碱性碱性岩系;火山喷发;斑岩铜矿;次生富集;民乐景谷;
- Keywords geophysics;Stratagem EH4 system;mineralization anomaly;hidden ore body;Cu-Ni deposit;porphyry Cu deposit;gold deposit; 地球物理;EH4连续电导率成像仪;矿化异常;隐伏矿体;铜镍矿床;斑岩铜矿;金矿床;
- Geological characteristics and prospecting mark of the Baishan porphyry Mo deposit, East Tianshan 东天山白山斑岩型钼矿床的地质特征及找矿标志
- The chemical symbol for copper is "Cu". 铜的化学符号是Cu。
- It's all over now so think mo more of it. 现在一切都过去了,因此别再去想它了。