The North China Craton (NCC) was clearly different from the Yangtze and Tarim cratons during the Late Mesoproterozoic to Early Neoproterozoic period because no distinct geological records have been found about the thermotectonic events related to assembly and breakup of the Rodinia Supercontinent. Therefore, various assumptions occur regarding relation between the NCC and the Rodinia. On the basis of the assumption, we propose a hypothesis (GOSEN joining hypothesis) that the Grenville Orogen, the southeastern margin of Siberia and eastern NCC were linked.