Xiaodushangxi tungsten deposit is located in the eastern end of the tarim plate, Beishan paleozoic continental margin activity with Liuyuan-Yu Well son with the western part of Rift Valley.

小独山西钨矿床位于塔里木板块的东端，北山陆缘活动带古生代柳园-俞井子裂谷带西段。

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The authors synthesized geological, geophysical and geochemical data, and believe that the plate tectonic setting of the study area should belong to the rift valley within the continental plate.

研究表明，本区火山活动应为大陆板块内部的裂谷环境，与消减带无关。 文中还总结了火山活动的时代、规模、顺序、碎屑锥特点。 研究了绳状、渣状熔岩的典型剖面、形成条件及流动方向。

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