|
Citation
|
González G, Fujita E, Shibazaki B, Hayashida T, Chiodini G, Lucchi F, Yokoyama I, Nemeth K, Mora-Amador R, Moya A, Chigna G, Martí J, Rouwet D. Sci. Rep. 2021; 11(1): e24489. |
|
Abstract
|
Correction to: Scientific Reports https://doi.org/10.1038/s41598-021-01725-1, published online 17 November 2021
The original version of this Article contained a repeated error in the Introduction, in Figure 1 and its accompanying legend, in the Results section under the subheading 'Stress changes caused by the earthquakes', in the Discussion and conclusions section under the subheading 'Volcanic eruptions long after the earthquakes', and in the Supplementary Information file, where the earthquake that occurred on November 7, 2012 was incorrectly mentioned as having occurred on November 11, 2012.
Corrected legend:
Epicenter of the 2012 earthquakes, volcanoes in states of unrest, and location of the seismic stations used to obtain the waveforms for calculating the dynamic stress of the earthquakes in Central America (more information in the Supplementary Material). The dashed line corresponds to the Meso-American trench along which the Cocos plate is subducting below the Caribbean plate. Grey circles indicate the seismic stations available for the three earthquakes in 2012 (August 27, El Salvador; September 5, Costa Rica; November 11, Guatemala). The yellow circles, black diamonds, and blue squares indicate the seismic stations that generated information for the El Salvador, Costa Rica and Guatemala earthquakes, respectively. The orange/white circles are the focal mechanism of each earthquake from Global CMT. The volcanoes analyzed in this study are: 1. Santa María, 2. Fuego, 3. Pacaya, 4. San Miguel, 5. San Cristóbal, 6. Telica, 7. Cerro Negro, 8. Momotombo, 9. Apoyeque, 10. Masaya, 11. Concepción, 12. Rincón de la Vieja, 13. Miravalles, 14. Tenorio, 15. Arenal, 16. Platanar, 17. Poás, 18. Irazú and 19. Turrialba. Figure created in Generic Mapping Tools (GMT; https://www.generic-mapping-tools.org/).
Language: en |