Abstract
The diagnostic minerals at the primary contact aureoles of the Phuket pegmatites indicate that there were dispersions of B, Mn and alkalis to their host rocks, both the metasedimentary rocks of the Phuket Group and the biotite-hornblende-muscovite granites. The contact aureoles of the pegmatitic segregations and their parental granites provide evidence that besides B, Mn, K and Na, specific metals such as Sn, Nb, Ta and W were also contributed in the late-stage fluids of the Phuket granite-pegmatite system.
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