| Citation: |
WANG Yan, QIN Tao, ZHANG Lidong, ZANG Yanqing, QIAN Cheng, ZHAO Chunqiang. Zircon U-Pb age evidence for the accretionary evolution of the Paleozoic Zalantun island arc in the northern part of the Great Xing'an Range[J]. Geological Bulletin of China, 2021, 40(12): 2186-2188.
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Zircon U-Pb age evidence for the accretionary evolution of the Paleozoic Zalantun island arc in the northern part of the Great Xing'an Range
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References
[1] Liu Y, Li W, Feng Z, et al. A review of the paleozoic tectonics in the eastern part of central asian orogenic belt[J]. Gondwana Research, 2017, 43: 123-148. doi: 10.1016/j.gr.2016.03.013 [2] 杨现力. 扎兰屯浅变质岩系地质特征及碎屑锆石年代学研究[D]. 吉林大学博士学位论文, 2007. [3] 苗来成, 刘敦一, 张福勤, 等. 大兴安岭韩家园子和新林地区兴华渡口群和扎兰屯群锆石SHRIMP U-Pb年龄[J]. 科学通报, 2007, 52(5): 591-591. doi: 10.3321/j.issn:0023-074X.2007.05.016 [4] 周建波, 王斌, 曾维顺, 等. 大兴安岭地区扎兰屯变质杂岩的碎屑锆石U-Pb年龄及其大地构造意义[J]. 岩石学报, 2014, 30(7): 1879-1888. [5] Qin T, Guo R R, Qian C, et al. Recognition of Early Paleozoic Magmatisms in the Supposed Proterozoic Basements of Zhalantun, Great Xing'an Range, NE China[J]. Acta Geologica Sinica, 2019, 93(3): 433-439. [6] Zhao C, Qin K Z, Song G X, et al. Early palaeozoic high-mg basalt-andesite suite in the duobaoshan porphyry cu deposit, NE China: constraints on petrogenesis, mineralization, and tectonic setting[J]. Gondwana Research, 2019, 71: 91-116. doi: 10.1016/j.gr.2019.01.015 -
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WANG Yan, QIN Tao, ZHANG Lidong, ZANG Yanqing, QIAN Cheng, ZHAO Chunqiang. Zircon U-Pb age evidence for the accretionary evolution of the Paleozoic Zalantun island arc in the northern part of the Great Xing'an Range[J]. Geological Bulletin of China, 2021, 40(12): 2186-2188.
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Figure 1.
Geotectonic location map and geological sketch map of Zhalantun area