MA Fang-fang, SUN Feng-yue, LI Bi-le, XUE Ming-xuan. ZIRCON U-Pb AGES OF DONGAN GOLD DEPOSIT IN HEILONGJIANG PROVINCE: Geological Implication[J]. Geology and Resources, 2012, 21(3): 277-280. DOI: 10.13686/j.cnki.dzyzy.2012.03.003
    Citation: MA Fang-fang, SUN Feng-yue, LI Bi-le, XUE Ming-xuan. ZIRCON U-Pb AGES OF DONGAN GOLD DEPOSIT IN HEILONGJIANG PROVINCE: Geological Implication[J]. Geology and Resources, 2012, 21(3): 277-280. DOI: 10.13686/j.cnki.dzyzy.2012.03.003

    ZIRCON U-Pb AGES OF DONGAN GOLD DEPOSIT IN HEILONGJIANG PROVINCE: Geological Implication

    • The age of the rhyolite porphyry, which is closely related to mineralization in Dongan gold deposit, is tested with LA-ICPMS zircon dating method. The results show that, the U contents of the rhyolite porphyry range from 269.1×10-6 to 956.0×10-6, while the Th contents, from 202.2×10-6 to 1276.8×10-6, with Th/U ratio between 0.43 and 1.80. The age of rhyolite porphyry is (109.6±1.7) Ma, which is synchronous with other epithermal gold deposits in the area. It implies the large-scale lithospheric extension and thinning in the late period of Early Cretaceous.
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