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嵩溪银锑矿是90年代初发现的一个大型新型独立银矿,其成因存在海底基性火山喷流和浅成中低温火山热液充填两种不同观点。前者认为成矿流体为海底热卤水,而后者则认为主要来自岩浆水,但有大气降水加入。较系统的N_2-Ar-He组成和He同位素研究清楚地显示嵩溪成矿流体主要来源于建造水或称沉积热卤水,其中幔源岩浆水的比例很小,一般<5％。从成矿流体来源看,嵩溪银锑矿成因类型应属沉积热卤水改造型。
The Songxi silver-antimony deposit is a large new type of independent silver deposit discovered in the early 1990s. Its origin includes two basic viewpoints: the basic volcanic jet of the seafloor and the filling of volcanic hydrothermal fluids into medium and low temperature. The former thought that the ore-forming fluid was submarine hot brine, whereas the latter considered it mainly from magmatic water but added with precipitation. The systematic N 2 -Ar-He composition and He isotope studies clearly show that the Songxi ore-forming fluid is mainly derived from built water or sedimentary hot brine, of which the proportion of mantle source magma water is very small, generally <5%. According to the sources of ore-forming fluids, the genetic type of Songxi silver-antimony ore belongs to the modified type of sedimentary hot brine.