The tectonic history of the Siberian continental plate is discussed here at the mainstages of geological chronicle: from Rodinia supercontinent, through Pangeasupercontinent, up to present-day position of Siberia within the structure of Eurasia. Westart from the end of Mesoproterozoic where the Rodinia supercontinent was assembled.The available geological and paleomagnetic data set suggests that at the Meso-Neoproterozoic boundary Siberian craton was a part of Rodinia supercontinentlengthening the Laurentia northward.
