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Richard Bono
Florida State UniversityMeeting roles in:
Plate tectonics commenced after formation of juvenile Paleoarchean to Mesoarchean continental crust
Late Permian core, surface and magnetosphere conditions revealed by single crystal paleointensities from the Emeishan large igneous province
Using Legendre Polynomial Based Paleosecular Variation Models to Infer Dynamo Dipolarity
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