中文摘要：

大地构造的进化，地区性地质的特征形成 andore 和控制矿石的结构上的研究证明了自从中生代， Da Hinggan Lingregion 进入了典型洲际 orogenic 阶段，它与披风羽毛活动有关仔细看起来是。Da Hinggan 石楠是典型披风分支结构并且在核心拥有明显的 magmatic 变形的建筑群，分开在圆周和重叠差错消沉盆滑动床。而且，所有这些是导致在这个区域控制的矿石形成和矿石的主要因素。这篇论文进一步也在 Da Hinggan 石楠的中间南部的片断探索矿化作用的机制，摘要矿化作用的规则，提出矿化作用的模型并且在未来时间指出矿石搜索取向。

英文摘要：

Studies on geotectonic evolution, regionally geological characteristics and ore-forming and ore-controlling structures have shown that since the Mesozoic the Da Hinggan Ling region has entered the typical intercontinental orogenic stage, which appears to be closely related to mantle plume activities. Da Hinggan Ling is a typical mantle branch structure and possesses obvious magmatie-metamorphie complexes in the core, detachment slip beds in the periphery and overlapped fault depression basins. Moreover, all these are the principal factors leading to ore formation and ore controlling in the region. This paper also further explores the mechanism of mineralization in the middle-southern segment of Da Hinggan Ling, summaries the rules of mineralization, puts forward the models of mineralization and points out the oresearch orientations in the future time.