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On the Late Hydrothermal Tungsten Deposits of Haiyangshan Mountain, Kuangsi

On the Late Hydrothermal Tungsten Deposits of Haiyangshan Mountain, Kuangsi

作     者:C. K.KUNG and J. H. CHANG (Geological Survey of China) 

出 版 物:《地质学报》 (Acta Geologica Sinica)

年 卷 期:1949年第Z1期

页      面:135-144页

主  题:Kuangsi On the Late Hydrothermal Tungsten Deposits of Haiyangshan Mountain 

摘      要:INTRODUCTIONThe Haiyangshan Mountain trending in the NNE-SSW direction is situated between the Hsiangan and Kuanyang cites in NE Kuangsi. The principal mines are located on the E slope at about 200 m above Sanyutsun, a village nearly 25 km NW of Kuanyang. The tungsten mineralization in the region is confined chiefly to the quartz veins which were formed by the ore-bearing solutions along the fractures in the granodiorite shortly after its consolidation.

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