The Baiyinnuo large and high-grade Pb-Zn deposit in Inner Mongolia is a representative skarn-type one. 内蒙古白音诺铅锌矿床是我国北方一个典型的矽卡岩矿床,具有大而富的特点。
The genesis of Keketale Lead-Zinc Deposit is discussed by means of its geological characters and geochemical characters, providing the basis for sulfide type Lead-Zinc deposit. 通过可可塔勒铅锌矿床地质特征及地球化学特征的研究,探讨可可塔勒铅锌矿床的成因,为寻找硫化物型铅锌矿提供了依据。