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对阿尔泰造山带南缘锡泊渡、阿拉托别和托斯巴斯陶等镁铁质岩体的主量元素和微量元素地球化学特征进行研究,并与喀拉通克岩体进行了对比。结果表明,这些岩体的形成过程与喀拉通克岩体不同,进而评价了这些岩体的找矿前景,提出锡泊渡北岩体具有较好的成矿条件,其他几个岩体成矿条件不十分理想。
The major and trace element geochemical characteristics of mafic rocks such as Xipudu, Alratose and Tuspastois on the southern margin of the Altay orogen were studied and compared with that of the Kalatongke. The results show that the formation process of these rock mass is different from that of the Kalatongk rock mass, and then the prospecting prospect of the rock mass is evaluated. It is suggested that the Xopudubei rock mass has better metallogenic conditions and other rock masses Mine conditions are not very satisfactory.