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Fig. 2 Conventional Late Cretaceous–Eocene reconstructions of the North Pacific realm. Conventional Late Cretaceous–Eocene reconstructions of the North.

Published byОлег Якимович Modified over 5 years ago

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Presentation on theme: "Fig. 2 Conventional Late Cretaceous–Eocene reconstructions of the North Pacific realm. Conventional Late Cretaceous–Eocene reconstructions of the North."— Presentation transcript:

1 Fig. 2 Conventional Late Cretaceous–Eocene reconstructions of the North Pacific realm.
Conventional Late Cretaceous–Eocene reconstructions of the North Pacific realm. In these reconstructions, the Pacific-Izanagi ridge persists at the northern edge of the Pacific plate until being subducted at ~55 Ma. The Pacific plate shows northerly motion from ~80 to 47 Ma (toward the Pacific-Izanagi ridge) and northwesterly motion after 47 Ma. Mantle reference frame reconstructions, plate boundaries, and velocities according to Müller et al. (15). Mathew Domeier et al. Sci Adv 2017;3:eaao2303 Copyright © 2017 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).

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