摘要
辽宁省的孔兹岩系主要分布于营口一草河口复向斜南北两翼，具有大致相同的岩石矿物组合、岩石化学及微量元素特征，经历了多期变形变质作用及混合岩化作用，具有同类的非金属矿产。
?The khondalite series in Liaoning Province distributed mainly in the both of south and northwings Yingkou and Caohekou composite downflod, and with almost same features of rock and mineral association, lithochemistry as well as microelements. They also underwent multitime deformation metamorphismand hybridization and have similar non-metallic minerals.
关键词
孔兹岩系
非金属矿产
辽宁
变质岩
Khondalite series Non-metallic minerals Liaoning Province
