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Laurentia Siberia A Precambrian continental reconstruction that places the rifted eastern margin of the Siberian craton against the rifted western margin of the Laurentian craton (Sears and Price, 1978, 2003) yields precise geologic matches between >20 crustal features. These range in age from 1.72 Ga to 550 Ma. The reconstruction model also provides a geologically viable rift/drift scenario for displacement of the Siberian craton from a Precambrian position adjacent to western Laurentia to its Paleozoic position adjacent to Europe.

SIGNIFICANT QUADRUPOLE MOMENT FOR PRECAMBRIAN GEODYNAMO? IMPLICATIONS FROM WEST LAURENTIA-SIBERIA CONTINENTAL RECONSTRUCTION AND NEPTUNIAN HOMOLOGUE