Note in proof: On October 9, as this article was being prepared for publication, a magnitude 7.6 earthquake occurred beneath the Jalisco region and caused significant loss of life and property. This earthquake highlights the societal need for accurate measurements of crustal strain rates in earthquake-prone zones. In the coming months, we plan to measure the amount of displacement that occurred within the GPS network during and after this earthquake
A very large earthquake took place on 28 March 1787 along the Mexican subduction zone. A unique char...
大地震とスロースリップの相互作用を解明 --メキシコにおける3つの大地震の連鎖的発生のメカニズム--. 京都大学プレスリリース. 2021-04-12.Either the triggering of...
The Cocos plate subducts beneath North America at the Mexico trench. The northernmost segment of thi...
Note in proof: On October 9, as this article was being prepared for publication, a magnitude 7.6 ear...
The October, 1995 Mw 8.0 Jalisco subduction earthquake has provided a thorough geodetic observation ...
We use coseismic displacements and aftershock information from Global Positioning System (GPS) measu...
On September 2017, two large earthquakes struck México. Numerous casualties and at least 40 building...
Surface waves from the 2017 Mw8.2 Tehuantepec earthquake remotely triggered tectonic tremors in the ...
The M = 8.1 Chiapas and the M = 7.1 Puebla earthquakes occurred in the bending part of the subducti...
We present evidence of fi ve late Holocene earthquake ruptures observed at two paleoseismological tr...
The October, 1995 Mw 8.0 Jalisco subduction earthquake has provided a thorough geodetic observation ...
Mexico City, a large megacity with over 21 million inhabitants, is exposed to several hazards, inclu...
The extensive damage to high‐rise buildings in Mexico City during the September 19, 1985 earthquake ...
We use coseismic displacements and aftershock information from Global Positioning System (GPS) measu...
Abstract. GPS measurements of crustal deformation in Guerrero, southern Mexico, include surveys coll...
A very large earthquake took place on 28 March 1787 along the Mexican subduction zone. A unique char...
大地震とスロースリップの相互作用を解明 --メキシコにおける3つの大地震の連鎖的発生のメカニズム--. 京都大学プレスリリース. 2021-04-12.Either the triggering of...
The Cocos plate subducts beneath North America at the Mexico trench. The northernmost segment of thi...
Note in proof: On October 9, as this article was being prepared for publication, a magnitude 7.6 ear...
The October, 1995 Mw 8.0 Jalisco subduction earthquake has provided a thorough geodetic observation ...
We use coseismic displacements and aftershock information from Global Positioning System (GPS) measu...
On September 2017, two large earthquakes struck México. Numerous casualties and at least 40 building...
Surface waves from the 2017 Mw8.2 Tehuantepec earthquake remotely triggered tectonic tremors in the ...
The M = 8.1 Chiapas and the M = 7.1 Puebla earthquakes occurred in the bending part of the subducti...
We present evidence of fi ve late Holocene earthquake ruptures observed at two paleoseismological tr...
The October, 1995 Mw 8.0 Jalisco subduction earthquake has provided a thorough geodetic observation ...
Mexico City, a large megacity with over 21 million inhabitants, is exposed to several hazards, inclu...
The extensive damage to high‐rise buildings in Mexico City during the September 19, 1985 earthquake ...
We use coseismic displacements and aftershock information from Global Positioning System (GPS) measu...
Abstract. GPS measurements of crustal deformation in Guerrero, southern Mexico, include surveys coll...
A very large earthquake took place on 28 March 1787 along the Mexican subduction zone. A unique char...
大地震とスロースリップの相互作用を解明 --メキシコにおける3つの大地震の連鎖的発生のメカニズム--. 京都大学プレスリリース. 2021-04-12.Either the triggering of...
The Cocos plate subducts beneath North America at the Mexico trench. The northernmost segment of thi...