CAJ | 학술논문

四川红卓铜矿是一个新发现的矿点，研究程度比较低．通过野外地质工作及室内综合分析，重新划定了矿区地层顺序，认为矿区构造为脆韧性和脆性2个层次．脆韧性变形以顺层剪切为特征，构造序列可确定为脆韧性顺层剪切→褶皱、逆冲断层→断层正滑．红卓铜矿在成矿特点上受构造影响明显，断层将矿区分为南西、中央、北东3个带，以中央带岩浆成矿作用显示最强．
사천홍탁동광시일개신발현적광점，연구정도비교저．통과야외지질공작급실내종합분석，중신화정료광구지층순서，인위광구구조위취인성화취성2개층차．취인성변형이순층전절위특정，구조서렬가학정위취인성순층전절→습추、역충단층→단층정활．홍탁동광재성광특점상수구조영향명현，단층장광구분위남서、중앙、북동3개대，이중앙대암장성광작용현시최강．
Hongzhuo copper deposit is a newly discovered mineralized point in Sichuan Province, it is in low research degree. Based on the field geological work and indoor comprehensive analysis, the stratigraphic sequence is re-established in mining area, and it is considered that there are two layers in ore area structure: ductile structure and ductile-brittle structure. Characteristic of ductile-brittle structure is shearing along layer. The structural sequence is ductile-brittle bedding shear to fold, thrust fault to normal fault. The mineralization of Hongzhuo copper deposit is obviously controlled by structure. The mining area was divided into three belts by faults: southwest, northeast and center belts, and center belt shows the strongest magmatic metallogenesis.