Saltar para: Post [1], Comentar [2], Pesquisa e Arquivos [3]

diariobombeiro



Quinta-feira, 11.10.12

Sismo de magnitude 5,7 registado no Chile

Um forte sismo de magnitude 5,7 na escala de Richter foi registado, esta quinta-feira, no centro do Chile e sentido na capital mas sem provocar estragos importantes, referiram os organismos especializados no Chile.

O abalo prolongado ocorreu às 14.23 horas locais (19.23 horas em Lisboa) e segundo as autoridades provocou numerosos cortes de eletricidade e de ligações telefónicas em diversas regiões de Santiago do Chile.

O Gabinete nacional chileno das situações de urgência (Onemi) precisou que o epicentro do sismo se situou nas regiões de Coquimbo (norte) e El Maule (sul), mas "não foi registada qualquer vítima nem danos de infraestruturas".

No centro de Santiago, forma evacuados diversos edifícios.

Fonte: JN

Tectonic Summary

Seismotectonics of South America (Nazca Plate Region)

The South American arc extends over 7,000 km, from the Chilean margin triple junction offshore of southern Chile to its intersection with the Panama fracture zone, offshore of the southern coast of Panama in Central America. It marks the plate boundary between the subducting Nazca plate and the South America plate, where the oceanic crust and lithosphere of the Nazca plate begin their descent into the mantle beneath South America. The convergence associated with this subduction process is responsible for the uplift of the Andes Mountains, and for the active volcanic chain present along much of this deformation front. Relative to a fixed South America plate, the Nazca plate moves slightly north of eastwards at a rate varying from approximately 80 mm/yr in the south to approximately 65 mm/yr in the north. Although the rate of subduction varies little along the entire arc, there are complex changes in the geologic processes along the subduction zone that dramatically influence volcanic activity, crustal deformation, earthquake generation and occurrence all along the western edge of South America.

Most of the large earthquakes in South America are constrained to shallow depths of 0 to 70 km resulting from both crustal and interplate deformation. Crustal earthquakes result from deformation and mountain building in the overriding South America plate and generate earthquakes as deep as approximately 50 km. Interplate earthquakes occur due to slip along the dipping interface between the Nazca and the South American plates. Interplate earthquakes in this region are frequent and often large, and occur between the depths of approximately 10 and 60 km. Since 1900, numerous magnitude 8 or larger earthquakes have occurred on this subduction zone interface that were followed by devastating tsunamis, including the 1960 M9.5 earthquake in southern Chile, the largest instrumentally recorded earthquake in the world. Other notable shallow tsunami-generating earthquakes include the 1906 M8.5 earthquake near Esmeraldas, Ecuador, the 1922 M8.5 earthquake near Coquimbo, Chile, the 2001 M8.4 Arequipa, Peru earthquake, the 2007 M8.0 earthquake near Pisco, Peru, and the 2010 M8.8 Maule, Chile earthquake located just north of the 1960 event.

Large intermediate-depth earthquakes (those occurring between depths of approximately 70 and 300 km) are relatively limited in size and spatial extent in South America, and occur within the Nazca plate as a result of internal deformation within the subducting plate. These earthquakes generally cluster beneath northern Chile and southwestern Bolivia, and to a lesser extent beneath northern Peru and southern Ecuador, with depths between 110 and 130 km. Most of these earthquakes occur adjacent to the bend in the coastline between Peru and Chile. The most recent large intermediate-depth earthquake in this region was the 2005 M7.8 Tarapaca, Chile earthquake.

Earthquakes can also be generated to depths greater than 600 km as a result of continued internal deformation of the subducting Nazca plate. Deep-focus earthquakes in South America are not observed from a depth range of approximately 300 to 500 km. Instead, deep earthquakes in this region occur at depths of 500 to 650 km and are concentrated into two zones: one that runs beneath the Peru-Brazil border and another that extends from central Bolivia to central Argentina. These earthquakes generally do not exhibit large magnitudes. An exception to this was the 1994 Bolivian earthquake in northwestern Bolivia. This M8.2 earthquake occurred at a depth of 631 km, making it the largest deep-focus earthquake instrumentally recorded, and was felt widely throughout South and North America.

Subduction of the Nazca plate is geometrically complex and impacts the geology and seismicity of the western edge of South America. The intermediate-depth regions of the subducting Nazca plate can be segmented into five sections based on their angle of subduction beneath the South America plate. Three segments are characterized by steeply dipping subduction; the other two by near-horizontal subduction. The Nazca plate beneath northern Ecuador, southern Peru to northern Chile, and southern Chile descend into the mantle at angles of 25° to 30°. In contrast, the slab beneath southern Ecuador to central Peru, and under central Chile, is subducting at a shallow angle of approximately 10° or less. In these regions of “flat-slab” subduction, the Nazca plate moves horizontally for several hundred kilometers before continuing its descent into the mantle, and is shadowed by an extended zone of crustal seismicity in the overlying South America plate. Although the South America plate exhibits a chain of active volcanism resulting from the subduction and partial melting of the Nazca oceanic lithosphere along most of the arc, these regions of inferred shallow subduction correlate with an absence of volcanic activity.

Preferred Location Parameters

ParameterValueUncertainty
Magnitude5.5 mb± 0.03
Location32.867°S, 70.401°W± 17.7 km
Depth81.9 km± 7.9 km
Number of Stations Used376
Number of Phases Used377
Minimum Distance40.1 km (0.36°)
Travel Time Residual0.82 sec
Azimuthal Gap63°
Review StatusREVIEWED
Event IDusb000d4jf
Fonte: USGS

Autoria e outros dados (tags, etc)

Tags:

por Diário de um Bombeiro às 21:30


Comentar:

CorretorEmoji

Se preenchido, o e-mail é usado apenas para notificação de respostas.



Mais sobre mim

foto do autor


Subscrever por e-mail

A subscrição é anónima e gera, no máximo, um e-mail por dia.

Pesquisar

Pesquisar no Blog  

calendário

Outubro 2012

D S T Q Q S S
123456
78910111213
14151617181920
21222324252627
28293031




Tags

mais tags