作者: D.W Russell , J.C van Moort
DOI: 10.1016/S0375-6742(99)00076-X
关键词: Quartz 、 Statistical analysis 、 Geology 、 Gold deposit 、 Vein (geology) 、 Reef 、 Mineralogy
摘要: The quartz veins of the Tasmania Reef (Beaconsfield) gold deposit are hypothermal origin. auriferous parts reef characterised by microcrystalline with on average 21 ppm As, 3 Ge and 14 Li in contrast barren which contain <2 <1 <3 Li. Further statistical analysis indicates that screening small samples (400 mg) for specific values their Al–Ge–Li–Na–Rb–Ca–Cl content is a useful indicator mineralisation quartz.