Abstract
According to new data of field observation, the youngest detrital zircon age and magmatic zircon age, four Precambrian blocks have been recognized in the Xing’an-Mongolia orogenic belt (XMOB), including the Erguna block (EB), Xing’an-Airgin Sum block (XAB), Songliao-Hunshandake block (SHB), and Jiamusi block (JB).
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Xu, B. (2015). Paleocontinents in Xing’an-Mongolia Orogenic Belt (XMOB). In: Zhai, M. (eds) Precambrian Geology of China. Springer Geology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-47885-1_12
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DOI: https://doi.org/10.1007/978-3-662-47885-1_12
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