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This research letter presents new paleomagnetic and geochronological data from the Xilinhot–Songliao Block (XSB) that clarifies its position at approximately 285 Ma, indicating it was situated on the northern margin of the East Paleo-Tethys Ocean (EPTO). The study reveals that the Hegenshan Ocean, located between the XSB and the Mongolia Block, was the primary ocean basin of the eastern Paleo-Asian Ocean during this period. These findings contribute to understanding the tectonic relationship between the Pal

Author

xiaoyao1997007

Language

EN