Figures
In Fig 4, the geometry of cross-sections B and C is incorrect. Please see the correct Fig 4 here.
A) Model of the crustal thickness (inversion of gravimetric data) along a NE-SW trending line from the trench to the Venezuela basin (location Fig 1C); B) Crustal strain pattern of the Northern Lesser Antilles; C) Restoration of the extensive deformation; D) Restoration of the compressive deformation.
Reference
- 1. Philippon M, Cornée J-J, Münch P, van Hinsbergen DJJ, BouDagher-Fadel M, Gailler L, et al. (2020) Eocene intra-plate shortening responsible for the rise of a faunal pathway in the northeastern Caribbean realm. PLoS ONE 15(10): e0241000. https://doi.org/10.1371/journal.pone.0241000 pmid:33079958
Citation: Philippon M, Cornée J-J, Münch P, van Hinsbergen DJJ, BouDagher-Fadel M, Gailler L, et al. (2021) Correction: Eocene intra-plate shortening responsible for the rise of a faunal pathway in the northeastern Caribbean realm. PLoS ONE 16(3): e0249163. https://doi.org/10.1371/journal.pone.0249163
Published: March 22, 2021
Copyright: © 2021 Philippon et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.