作者: Zhen-Zhen Li , Ke-Zhang Qin , Guang-Ming Li , Lu-Ying Jin , Guo-Xue Song
DOI: 10.1016/J.JSEAES.2018.06.020
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摘要: Abstract To constrain the pre-mineralization tectonic evolutionary history and nature of magma source Chalukou Mo deposit, which is located on western margin Xing’an block, we recognized studied a period Neoproterozoic magmatism suite Early Paleozoic volcanic rocks in this ore district. The magmatic zircons quartz chlorite schist collected from Wolegen Group yielded concordant 206Pb/238U age 685.1 ± 4.5 Ma (MSWD = 0.21), they show very high eHf(t) values (+15.5 to +17.3) young Hf modal ages (573–664 Ma) close formation age, indicating that protolith was generated during Neoproterozoic, most likely derived depleted mantle region. This might represent an important crustal growth event within Block. host wallrocks deposit mainly consist rhyolite, dacite, andesite tuff have undergone slight deformation metamorphism. results zircon LA-ICP-MS U-Pb dating indicated were 472–475 Ma. whole-rock geochemical analysis indicate arc-affinity features characterized by LREE enrichment with moderate strong fractionation between HREE (LaN/YbN = 7.7–13.6), intense negative Eu anomalies (δEu = 0.36–0.71), pronounced positive Ba, Th, U, Pb La Nb-Ta, P Ti anomalies. isotopes various eHf (t) ranging −2.0 +5.9 slightly old two-stage model 1070 Ma 1573 Ma. Combined discrimination diagrams, these data partial melting older lower crust addition juvenile component active continental setting related subduction Paleo-Asian Ocean Songliao blocks. existence activity Mesoproterozoic materials obtained district demonstrated Precambrian basement exists Block, but its distribution area may be limited. As largest porphyry China, ore-forming multiple sources, considering long-term events occurred under different settings previous modification refertilization and/or lithospheric generation fertile crust, direct ore-related porphyries.