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近二、三十年来,国內外鎢矿床成因分类的基本情况是:对外生鎢矿床没有原則性的爭論;而对內生鎢矿床則存在着原則性的分歧:林格崙的溫度-压力准則,多年来为多数分类者所采用。部分分类者又采用了C.C.斯米尔諾夫的錫矿成因分类准則。此外,还存在着其他一般性內生金属矿床分类的分歧意見,其中也涉及到鎢矿床成因类型的划分問題。
In the past two or three decades, the basic classification of genesis of tungsten deposits at home and abroad is as follows: there is no principle debate on exogenous tungsten deposits; and there are principle differences on endogenous tungsten deposits: the temperature-pressure principle of Ringgren , Adopted by most taxonomies over the years. Some of the taxonomies also adopted the C.C. Smirnov classification of tin genesis. In addition, there are still different opinions on the classification of other general endogenic metal deposits, which also involves the classification of genetic types of tungsten deposits.