///Huxingshan W-Be deposit is a supergiant W-Be deposit which has just been discovered in recent years. Through comparison with regional strata and strata mineralization trace element analysis, this paper verifies that in the mining area the main ore-bearing strata is Niutitang Formation of Lower Cambrian system instead of Doushantuo Formation of Sinian system which was mistaken as the right strata for many years. After looking at the strata in a whole new way, the author believes that the main ore-forming material source in Huxingshan mining area is deep concealed intrusive magmatic rock, and it has nothing to do with metallogenic specialization of strata. Furthermore, the initial judgment of the genesis of Huxingshan tungsten deposit can be regarded as guidance to prospection in the area in the future.
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