本文主要介绍了根据这种原则在新疆北山成矿带内进行铜镍矿床预测时，所建立的矿床地质概念模型。
For the statistical prediction of the copper - nickel deposit in Xinjiang Beishan minerogenetic belt, we have established the geological conceptual model of mineral deposits.
在此基础上对控制成矿带、矿田及矿床的构造特征进行了分析，总结了带内矿床定位的两类构造组合形式。
After analyzing structure characteristics controlling metallogenic belt, ore field, and deposits, two structure assemblage styles for ore depositing have been summarized.
喀拉通克铜镍硫化物矿床是产于我国北疆喀拉通克成矿带内的大型岩浆铜镍硫化物矿床。
The Karatungk magmatic Cu-Ni sulfide deposit exists in the Karatungk metallogenic belt in northern Xinjiang in China.
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