云英岩化的黑云母中含有辉钼矿,辉钼矿与黑云母相伴生,辉钼矿为鳞片状,部分发生弯曲,黑云母具有膝折现象。花岗斑岩与钼矿关系密切,钼矿体多产在花岗斑岩的下盘或接触带附近,钼矿化多呈大脉状、网脉状(脉宽1~10 cm不等)及团块状(粉状),多与围岩的片理、片麻理(或层理)一致或斜交,并有相互交切现象,说明这些单...
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