摘要
巴依达勒斯铅多金属矿预查区位于诺尔特复向斜东南段内。断裂是区域内的主要构造,其次为褶皱,出露岩性以侵入岩为主。对测区进行了1:25000岩石地球学测量结果分析,并根据元素异常强度最终圈定两个乙类异常区:A-乙1异常位于巴依达勒斯铅多金属矿测区北部,A-乙2异常位于其中南部,两者异常强度均较高,这对后期研究该区域的找矿或地质问题具有重要作用。
The Bayidalesi Zinc Polymetallic Deposit is located in the southeast of Nurt synclinorium. Regional features is characterized by fractures, folds and intrusive rocks in the explored area. Geochemical survey with a scale of 1：25000 has been carried out in this area. And according to the anomaly intensity of elements, two anomalies＇ parts with Class B（strong anomalies） were delineated： one is in the north and the other is in the central south of the survey region. What we got from these element anomalies of this region has some significant meanings for the future prospecting work.
出处
《四川有色金属》
2017年第3期9-12,共4页
Sichuan Nonferrous Metals
关键词
铅多金属矿
诺尔特复向斜
地球化学测量
异常强度
zinc polymetallic deposit
Nurt synclinorium
geochemical survey
anomaly intensity
