Progressive accretion in the Middle America Trench, Southern Mexico

Nature ◽  
1979 ◽  
Vol 281 (5733) ◽  
pp. 638-642 ◽  
Author(s):  
J. Casey Moore ◽  
Joel S. Watkins ◽  
Thomas H. Shipley ◽  
Steven B. Bachman ◽  
Floyd W. Beghtel ◽  
...  
1982 ◽  
Vol 10 (1) ◽  
pp. 107-119 ◽  
Author(s):  
Kenneth J. McMillen ◽  
Robert H. Enkeboll ◽  
J. Casey Moore ◽  
Thomas H. Shipley ◽  
John W. Ladd

1982 ◽  
Vol 10 (1) ◽  
pp. 77-94 ◽  
Author(s):  
J. Casey Moore ◽  
Joel S. Watkins ◽  
Kenneth J. McMillen ◽  
Stephen B. Bachman ◽  
Jeremy K. Leggett ◽  
...  

1989 ◽  
Vol 11 (1) ◽  
pp. 69-76 ◽  
Author(s):  
R. M. Prol-Ledesma ◽  
V. M. Sugrobov ◽  
E. L. Flores ◽  
G. Ju�rez M. ◽  
Ya. B. Smirnov ◽  
...  

2021 ◽  
Author(s):  
Alejandro Ramírez-Rojas ◽  
Elsa Leticia Flores-Márquez

<p>After the M8.2 earthquake occurred on September 07, 2017 at Isthmus of Tehuantepec, notable spatial and temporal changes where<br>registered, the temporal rate of occurrence increased and the spatial seismicity distribution showed a clear clusterization along<br>the region of collision of the Tehuantepec Transform/Ridge with the Middle America Trench off Chiapas. Also, the b-value in the<br>Gutenberg-Richer law showed changes in time. On the basis of that behavior we studied the sequence of magnitudes of the<br>earthquakes occurred within the Isthmus of Tehuantepec at southern Mexico from 2010 to 2020, by using the nowcasting method<br>and the multifractal detrended fluctuation analysis. Our findings suggest the b-value could depend on time and after the main-shock<br>M8.2, the underlying dynamics in the Tehuantepec ridge has been changed, which is clearly described by our analyses based on<br>nowcasting method and in the multifractality estimated changes.</p>


Sign in / Sign up

Export Citation Format

Share Document