Abstract
This chapter presents the application of the QRV method to dynamic restoration of the thermal state of the mantle beneath the Japanese islands and their surroundings. The geodynamic restoration for the last 40 million years is based on the assimilation of the present temperature inferred from seismic tomography, and the present plate movement derived from geodetic observations, paleogeographic and paleomagnetic plate reconstructions.
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Ismail-Zadeh, A., Korotkii, A., Tsepelev, I. (2016). Application of the QRV Method to Modelling of Plate Subduction. In: Data-Driven Numerical Modelling in Geodynamics: Methods and Applications. SpringerBriefs in Earth Sciences. Springer, Cham. https://doi.org/10.1007/978-3-319-27801-8_6
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DOI: https://doi.org/10.1007/978-3-319-27801-8_6
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