Abstract
The Qianlishan granite, which is closely related to the Shizhuyuan tungsten polymetallic mineralization, is aluminous alkali-type granite. The intimate temporal and spatial association among the basaltic, syenite and granitic rocks in the mining area, and their major and trace elements, and Nd, Pb, Sr, O isotopic compositions indicate that the crustal-mantle interaction probably was an important constraint on, and participated in, the formation of the superlarge ore deposit.
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Zhao, Z., Bao, Z., Zhang, B. et al. Crust-mantle interaction and its contribution to the Shizhuyuan superlarge tungsten polymetallic mineralization. Sci. China Ser. D-Earth Sci. 44, 266–276 (2001). https://doi.org/10.1007/BF02882261
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DOI: https://doi.org/10.1007/BF02882261