1) porphyry molybdenum deposit
斑岩型钼矿
1.
In recent years work of geology and physical general survery in the molybdenum (gold,silver) ore district of Xin County Wuchenghe Fengxiang mountain, find obvious IP anomaly, Drawed the trinity prospecting model of porphyry molybdenum deposit-structure, porphyry, IP anomaly.
经钻探验证,揭示了风响山钼矿化带,得出了斑岩型钼矿“三位一体”——构造、斑岩体、激电异常的找矿模式。
2.
The Wenquan porphyry molybdenum deposit in West Qinling area occurs in Indosinian complexes,with the wall rocks being K-rich calc-alkaline rocks.
温泉斑岩型钼矿床产出于印支期复式杂岩体中。
3.
Based on regional mineralizing background,mine geology,geochemical and geophysical exploration,ore genesis and ore-forming conditions,ore prospecting and significance in the Dasuji porphyry molybdenum deposit are briefly reviewed.
主成因类型属低品位斑岩型钼矿床,有可能发展为中型矿床。
4) porphyry molybdenum deposit
斑岩型钼矿床
1.
The paper focuses on the features,criteria for ore prospecting and prospecting method of the Fu anpu middle porphyry molybdenum deposit,Shulan City,which has an important guiding significance for prospecting large,middle porphyry molybdenum deposit in Indo-Sinian-Yanshan granites in the Shulan-Jiaohe area,northern part of Jilin Provinc
本文较详细地介绍了福安堡中型斑岩钼矿床的地质特征、找矿标志及找矿方法,对在吉林地区北部舒兰—蛟河一带分布的印支—燕山期花岗岩区寻找大、中型斑岩型钼矿床具有重要的指导意义。
5) Wenquan porphyry Mo deposit
温泉斑岩型钼矿
6) Donggou porphyry Mo deposit
东沟斑岩型钼矿
1.
The Donggou porphyry Mo deposit, located in Ruyang County of Henan Province, is a giant ore deposit discovered in recent years.
河南汝阳东沟斑岩型钼矿是近年来发现的超大型钼矿床,含钼斑岩被认为是太山庙岩基的岩枝或晚期分异产物。
补充资料：彩钼铝矿
分子式：
分子量：
CAS号：
密度：6.3～7.0
性状：四方晶系，晶体呈四方半状，集合体呈粒状块体。通常呈蜡黄、黄、黄褐等色，条痕白色，具有金刚光泽。
制备或来源：产于铅锌矿床的氧化带中，大量聚积可作为铅和钼的矿石利用。
分子量：
CAS号：
密度：6.3～7.0
性状：四方晶系，晶体呈四方半状，集合体呈粒状块体。通常呈蜡黄、黄、黄褐等色，条痕白色，具有金刚光泽。
制备或来源：产于铅锌矿床的氧化带中，大量聚积可作为铅和钼的矿石利用。
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