CAJ | 학술논문

成矿单元是成矿意义上的地质单元。笔者在继承全国矿产资源潜力评价项目发布的中国成矿单元Ⅰ级(成矿域)、Ⅱ级(成矿省)、Ⅲ级(成矿区带)最新划分方案的基础上，对秦岭地区5个Ⅲ级成矿单元(成矿区带)界线进行修正，以较明显的地层、构造和岩浆带特征及相关的主成矿作用为标志，划分15个Ⅳ级成矿单元(成矿亚区带)，并概述各Ⅳ级成矿单元的地质矿产特征。
성광단원시성광의의상적지질단원。필자재계승전국광산자원잠력평개항목발포적중국성광단원Ⅰ급(성광역)、Ⅱ급(성광성)、Ⅲ급(성광구대)최신화분방안적기출상，대진령지구5개Ⅲ급성광단원(성광구대)계선진행수정，이교명현적지층、구조화암장대특정급상관적주성광작용위표지，화분15개Ⅳ급성광단원(성광아구대)，병개술각Ⅳ급성광단원적지질광산특정。
Metallogenic unit is a geological unit on thein terms of metallogenic significance.The latest classification scheme about Chinese metallogenic units released by the national mineral resource potential assessment project includes Level I (Metallogenic domain ), Level II (metallogenic provinces)and Level III (metallogenic belts).This article revises boundaries of the five Level III metallogenic units (metallogenic belts)in the Qinling area on the basis of the inheritance of this previous classification scheme.Then the five Level III metallogenic units are divided into 15 Class IV metallogenic units (metallogenic sub-zones))as a symbol of according to significant stratigraphic, tectonic and magmatic belt characteristics and as well as relevant majorassociated mineralization .Furthermore,there is a summary about geology and mineral characteristics features of every Class IV metallogenic unit (metallogenic sub-zones ) are summarized in this paper.