Registros del 1 al 10 de 26 encontrados |
![](./images/clear.gif) 1.- A tremor and slip event on the Cocos-Caribbean subduction zone as measured by a global positioning system (GPS) and seismic network on the Nicoya Peninsula, Costa Rica
American Geophysical Union; Washington, DC; USA; United States, 2010
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![](./images/clear.gif) 2.- ANALYSIS OF THE 8/20/99 MW 6.9 COSTA RICA UNDERTHRUSTING EARTHQUAKE AND AFTERSHOCKS
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2000
AGU 2000 FALL MEETING
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![](./images/clear.gif) 3.- CHARACTERISTICS OF THE NICOYA PENINSULA, COSTA RICA SEISMOGENIC ZONE FROM FOCAL MECHANISM DETERMINATIONS
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002
AGU 2002 FALL MEETING
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![](./images/clear.gif) 4.- CONTROL OF SEAFLOOR ROUGHNESS ON EARTHQUAKE RUPTURE BEHAVIOR
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2003
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![](./images/clear.gif) 5.- Correlated transient fluid pulsing and seismic tremor in the Costa Rica subduction zone
Elsevier; Amsterdam; NLD; Netherlands, 2005
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![](./images/clear.gif) 6.- Crustal thickness and depth to the subducting slab underneath northern Costa Rica based on receiver function analysis
MARGINS Office;; USA; United States, 2008
The next decade of the Seismogenic Zone Experiment; abstract volume
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![](./images/clear.gif) 7.- Distinct updip limits to geodetic locking and microseismicity at the northern Costa Rica seismogenic zone; evidence for two mechanical transitions
Columbia University Press;; USA; United States, 2007
The seismogenic zone of subduction thrust faults
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![](./images/clear.gif) 8.- Earthquake relocation and focal mechanism determination using waveform cross correlation, Nicoya Peninsula, Costa Rica
Seismological Society of America; Berkeley, CA; USA; United States, 2006
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![](./images/clear.gif) 9.- EVIDENCE FOR A THERMALLY CONTROLLED SEISMOGENIC UPDIP LIMIT FOR SUBDUCTION AT NICOYA, COSTA RICA
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002
AGU 2002 FALL MEETING
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![](./images/clear.gif) 10.- EVIDENCE FOR SERPENTINIZATION OF THE FOREARC MANTLE WEDGE ALONG THE NICOYA PENINSULA, COSTA RICA
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2004
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