CAJ | 학술논문

大水沟碲矿床具有良好的多金属矿集区的区域成矿地球化学背景。研究表明大水沟碲矿床碲成矿物质可能源于深部，且与小金河-箐河等深大断裂有密切联系。
대수구제광상구유량호적다금속광집구적구역성광지구화학배경。연구표명대수구제광상제성광물질가능원우심부，차여소금하-정하등심대단렬유밀절련계。
This paper deals with regional geochemical characteristics of the Dashuigou Te deposit in Shimian, Sichuan which are:geochemical background rich in iron-group elements, as well as Cu、Zn、Hg、Mo、Sb、F、Pb、Au and Ag with depletion in SiO2 and K2O and the Te deposit lying in the intensive turning of the steep zones in Pb-isotope (V2) isograms and in Te-depleted geochemical background with local Te enrichment (up to 7-8 orders of magnitude). They suggest that the ore-forming metals might be derived from the depth. The ore-formation should be associated with the Xiaojinhe-Jinghe deep fracture zone.