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Temas de Sismología e Ingeniería Sísmica (curso 2007-2008)
Presentación de los diferentes temas de la asignatura de Sismología e Ingeniería ...
Giner Caturla, José Juan
core +1 more source
The Oaxaca Mexico, earthquake of 29 november 1978: a preliminary report on aftershocks
El área de réplicas del período del 1 o. al 12 de diciembre de 1978 para el temblor de Oaxaca (29 de noviembre, 1978; Ms= 7.8) se estima en 6000 km2. El temblor· parece llenar el tramo de quietud sísmico entre los temblores de 196.5 (Ms =7.6) y .1968 ...
S. K. Singh +5 more
doaj +1 more source
Refining the Eruption Chronology of Atitlán Caldera Through Zircon Double‐Dating
Abstract Precise dating of Quaternary volcanism is vital for risk mitigation, understanding volcano‐climate interactions, and deciphering the evolution of large silicic magmatic systems. The Atitlán caldera in Guatemala has experienced major eruptions that challenge radiometric dating techniques and complicate eruption chronology in this densely ...
Alejandro Cisneros de León +7 more
wiley +1 more source
The 29 november, 1978, Oaxaca earthquake: foreshock activity
El análisis de la .actividad sísmica (m≥2.8) registrada por medio de una red local de 6 sismográfos durante 3 semanas previas a la ocurrencia de un fuerte temblor (29 de. Noviembre de 1978, Ms=7.8) en Oaxaca-, revela los siguientes aspectos (Ponce et al.,
L. Ponce +4 more
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Abstract Observations of seismic waves that have passed through the Earth's lowermost mantle provide insight into deep mantle structure and dynamics, often on relatively small spatial scales. Here we use SKS, S2KS, S3KS, and PKS signals recorded across a large region including the United States, Mexico, and Central America to study the deepest mantle ...
Jonathan Wolf +5 more
wiley +1 more source
Focal mechanism of six large earthquakes in northern Oaxaca, Mexico, for the period 1928-1973
Con el fin de ayudar a comprender el neotectonismo en la región norte de Oaxaca, se estudiaron 6 temblores fuertes (mb≥6.5) de profundidad intermedia que ocurrieron durante los últimos 50 años (1928-1973) en dicha región.
Z. Jiménez, L. Ponce
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Abstract The Central Apennine Fault System (CAFS) characterizes an active tectonic region of significant importance, witnessing numerous destructive seismic events over the last millennia. Although numerous studies have underscored the role of Coulomb stress transfer (CST) in initiating some of the most catastrophic earthquakes, investigations focusing
G. Valentini +3 more
wiley +1 more source
Source mechanism of the november 29, 1978, Oaxaca, Mexico earthquake - a large simple event
El reciente temblor de Oaxaca, México (Ms = 7.8) es de especial interés pues se localiza dentro de un tramo de quietud (“gap”) sísmica determinado previamente.
Gordon S. Stewart, Eric P. Chael
doaj +1 more source
Mechanical Energy Dissipation During Seismic Dynamic Weakening in Calcite‐Bearing Faults
Abstract Earthquakes are frictional instabilities caused by the shear stress decrease, that is, dynamic weakening, of faults with slip and slip rate. During dynamic weakening, shear stress depends on slip, slip rate, and temperature, according to constitutive laws governing the earthquake rupture process.
Stefano Aretusini +8 more
wiley +1 more source
Subduction of the Cocos Plate and deep active fracture zone of Mexico.
La morfología y los parámetros de la zona de Wadati-Benioff fueron identificados a base de la distribución de los focos de terremotos en la región de México.
Václav Hanus, Jiri Vanek
doaj +1 more source

