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本文所引述的是东喀尔貝含錫黑鎢矿脈中黑鎢矿、白鎢矿与黃铁矿之間相互共生关系的一些有兴趣的資料,其矿物間的相互关系常成为推測成矿作用的依据。在叙述上述矿物間相互关系之前,首先談談喀尔貝含锡黑鎢矿床的一般情況。在喀尔貝的石英脈黑鎢矿床是一般常見的大型脈狀矿床,黑鎢矿化不均匀,常呈巢狀产出。圍岩主要是上二叠紀花崗岩,矿脈与花崗岩的接触处受到了强烈的云英岩化作用。該区含錫黑鎢矿脈矿床中的矿物成份均相类似,其中主要矿
This paper quotes some interesting data on the symbiotic relationship between wolframite, scheelite and pyrite in the Dongkalbei tin-wolframite vein. The inter-mineral relationship is often the presumed mineralization The basis of the role. Before describing the interrelationships between the above minerals, we first talk about the general situation of the Carburite-containing wolframite deposit. Quartz veins wolframite deposits in Carbere are common large-scale vein-like deposits. Uranium mineralization is uneven, and often nested. Surrounding rock is mainly Upper Permian granite, veins and granite contact has been strongly cloud-type lithification. The tin-bearing wolframite veins in the area of mineral composition are similar, including the main ore