Long-term Crustal Uplift Rates in Kanto District due to Steady
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erm Crustal Uplift Rates in Kanto District due to S duction of the Pacific and the Philippine Sea Plate (a) The crustal uplift rates com puted from a steady plate subduction model. (b) The crustal uplift rates es timated from the present heights of marine t erraces.
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Long-term Crustal Uplift Rates in Kanto District due to Steady Subduction of the Pacific and the Philippine Sea Plates. (a) The crustal uplift rates computed from a steady plate subduction model. (b) The crustal uplift rates estimated from the present heights of marine terraces. - PowerPoint PPT Presentation
Transcript of Long-term Crustal Uplift Rates in Kanto District due to Steady
Long-term Crustal Uplift Rates in Kanto District due to Steady Subduction of the Pacific and the Philippine Sea Plates
(a) The crustal uplift rates computed from a steady plate subduction model.
(b) The crustal uplift rates estimated from the present heights of marine terraces.
