CAJ | 학술논문

将成矿系列理论同成矿地质背景研究相结合，为阐明区域成矿规律奠定基础。借鉴我国地质学家创立的矿床成矿系列理论，据地质建造和成矿特征，按成矿系列与地质建造时间关系，将准噶尔北缘的北准噶尔成矿带（Ⅲ-3）、唐巴勒-卡拉麦里成矿带（Ⅲ-4）和准噶尔盆地（Ⅲ-5）成矿系列细化为“同生”、“准同生”、“后生”、“表生风化”等，并将同一套地质建造相关的几个世代成矿系列构成一个成矿系列家族。对成矿系列进行深化研究，初步确定14个成矿系列家族和17个成矿系列。
장성광계렬이론동성광지질배경연구상결합，위천명구역성광규률전정기출。차감아국지질학가창립적광상성광계렬이론，거지질건조화성광특정，안성광계렬여지질건조시간관계，장준갈이북연적북준갈이성광대（Ⅲ-3）、당파륵-잡랍맥리성광대（Ⅲ-4）화준갈이분지（Ⅲ-5）성광계렬세화위“동생”、“준동생”、“후생”、“표생풍화”등，병장동일투지질건조상관적궤개세대성광계렬구성일개성광계렬가족。대성광계렬진행심화연구，초보학정14개성광계렬가족화17개성광계렬。
According to the temporal relationship between geological formation and metallogenic series, in reference to the theory“metallogenic series”,founded by Chinese geologists,in view of geological formation and metallogenic charac-teristics, the metallogenic series of the north Junggar metallogenic belt (Ⅲ-3) ,the Tanggubale-Kalamaili metallogenic belt (Ⅲ-4) and the Junggar Basin (Ⅲ-5), which are located in The north Margin of Junggar, are meticulously classified into syngenetic, parasyngenetic, epigenetic and superficial weathering types in order to combine the theory“metallogen-ic series”and the metallogenic geological background study, lay a good foundation for clarifying regional metallogenic regularity. Many metallogenic series with the same geological formation and different generations comprise a family. In this study, the metallogenic series on the north Margin of Junggar preliminary are classified into 14 families and 17 metallogenic series.