The Oligocene Yao-an syenite porphyry, associated with gold mineralisation, and the Machangqing alkali granite porphyry-monzonite porphyry, associated with Cu mineralisation, belong to the Red River-Jinshajiang alkaline igneous belt that formed in a continental setting in southwestern China. A study of the mineral chemistry of major silicate minerals in these two mineralised intrusions provides insights into their overall crystallisation conditions. The temperature and pressure conditions, derived from amphibole-plagioclase and perthite-plagioclase geothermometry and Al-in-amphibole barometry, suggest that the Yao-an intrusion crystallised at around 820 ± 50°C and 0.9-1.3 kbar, whereas the Machangqing intrusion crystallised at around 730 ± 50°C and 2.2-2.8 kbar. The higher temperature and lower pressure of crystallisation for the Yao-an intrusion relative to the Machangqing intrusion indicates that it was emplaced at a shallower crustal level. Based on biotite composition, the two intrusions formed under imposed oxygen fugacities above the Ni-NiO buffer (NNO), and the Yao-an intrusion crystallised under more oxidising conditions than the Machangqing intrusion. The results show that the intrusions associated with Cu-Au mineralisation in the Red River-Jinshajiang alkaline igneous belt were emplaced at a relatively high fO2, which, together with the weakly fractionated magma, favoured Au enrichment relative to Cu in the belt.

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Persistent URL dx.doi.org/10.1007/s00710-009-0047-4
Journal Mineralogy and Petrology
Citation
Xianwu, B. (Bi), Ruizhong, H. (Hu), Hanley, J.J. (J. J.), Mungall, J.E, Jiantang, P. (Peng), Linbo, S. (Shang), … Xiaoyan, H. (Hu). (2009). Crystallisation conditions (T, P, f O2) from mineral chemistry of Cu- and Au-mineralised alkaline intrusions in the Red River-Jinshajiang alkaline igneous belt, western Yunnan Province, China. Mineralogy and Petrology, 96(1-2), 43–58. doi:10.1007/s00710-009-0047-4