摘要
哈巴特盖测区1/5万土壤地球化学测量发现了4个异常区,多元素组合异常多分布在黑云母二长花岗岩的内、外接触带上,土壤地球化学异常特征显示本区成矿是多期次的,多元素组合异常在露头矿和盲矿上方均有出现,且异常连续、浓集中心明显,异常的强度和规模大,呈带状、宽带状或面状产出。
Four anomaly areas are delineated by soil geochemical survey at 1：50,000 scale in Habategai area. Composite poly-element anomalies are distributed along inner-contact zone and outer-contact zone of biotite-monzonitic granite. Judged from the characteristics of soil geochemical anomaly the ore forming processes is characteristic of poly-epochs and poly-stages. Poly-element composite anomalies are found above surface ores and blind ores. Anomalies are big and continuous in belt, zone or area with clear concentration centers.
出处
《地质找矿论丛》
CAS
CSCD
2006年第B10期144-148,共5页
Contributions to Geology and Mineral Resources Research
关键词
哈巴特盖银多金属矿
土壤地球化学异常特征
组合异常
异常强度
浓集中心
内蒙古
Habategai soil geochemical anomaly characteristics
composite anomaly
anomaly intensity
concentration center,east Ujimqin
Inner Mongolia
