The Sikhote-Alin orogenic belt is a key area for understanding the evolution of the lithospheric plate interaction in the East Asian paleocontinent margin. At the same time, only limited and fragmentary precision isotope–geochemical and geochronological data are available for this region. New age data on the Early Paleogene magmatism supplement the available material and substantiate a specific Middle Paleocene–Early Eocene magmatic stage (60.5–53.0 Ma) dominated by A-type acid rocks in the southern Russian Far East during the geodynamic reconstruction of the continental margin.

中文翻译：

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俄罗斯南部远东地区中新世-早始新世（60.5-53.0 Ma）岩浆期

锡科特－阿林造山带是了解东亚古大陆边缘岩石圈板块相互作用演化的关键领域。同时，该地区只有有限的，零碎的精确同位素地球化学和年代学数据。古近纪早期岩浆作用的新纪元数据补充了可用的资料，并证实了俄罗斯南部远东地区大陆动力学重建期间以A型酸性岩石为主的特定的古新世-早始新世岩浆阶段（60.5-53.0 Ma） 。