摘要
东升庙是华北地台北缘西段的一个特大型铅锌硫矿床。在对矿床区域成矿地质条件和矿床地质地球化学特征分析研究的基础上,提出海底喷流沉积成因观点,并初步探讨了矿床海底喷流沉积成矿作用机理。
The Dongshengmiao superlarge Pb-Zn-S deposit is situated on the Inner Mongolia axis in the North China Platform. There has been no unity of thinking, even up to now, on its me-tallogenesis. In this paper the deposit is suggested to be of the submarine exhalative-sedimen-tary metallogenic type based on its regional geological setting and geological-geochemical characteristics of the deposit. The metallogenic mechanism of this deposit is also discussed in this paper.
出处
《地球化学》
CAS
CSCD
北大核心
1992年第4期375-382,共8页
Geochimica
