钨矿床 meaning in Chinese

tungsten deposit

The occurrence state and synthesis utilization of accompanying silver in tungsten deposit of china
我国钨矿床中伴生银的赋存状态及其综合利用
Generally magmatic hydrothermal cu and au deposits enrich cl and s , but w and sn deposits are rich f systems . in this paper , in order to study the relationship between the cu , w and
本文以著名的江西德兴铜厂超大型斑岩铜矿床和大吉山钨矿床作为研究对象，研究f 、 cl与w 、 cu成矿的关系。
Log ( fh2o / fhcl ) fluid and log ( fhf / fhcl ) fluid ) , tongchang porphyry copper deposit system is enriched in chlorine , however dajishan tungsten deposit system is relatively enriched in fluorine , which transport w , sn , nb , ta , et al . ( 8 ) according to the characters of the porphyry copper deposits , copper is transported by chlorine , such as cucl0 and cucl2
忍l ) flu ， d 、 109 ( / hr州el ) fluid )发现，铜厂斑岩型铜矿床的成矿体系是相对富氯体系，而大吉山石英脉型钨矿床成矿体系相对富氟，同时氟可能主要迁移w 、 sn 、 nb 、 ta等金属元素。