Seismicity in Costa Rica during 2013
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Keywords

Sismología
RSN
sismicidad del 2013
fuentes sísmicas
Costa Rica Seismology
RSN
seismicity in 2013
seismic sources
Costa Rica

How to Cite

Linkimer, L., Porras, J. L., Barquero, R., Araya, M. C., Lücke, O. H., Taylor, M., & Rojas, W. (2014). Seismicity in Costa Rica during 2013. Revista geológica De América Central, 51. https://doi.org/10.15517/rgac.v51i1.17043

Abstract

During 2013, the National Seismological Network (RSN: UCR-ICE) located 2547 earthquakes and reported 261 felt events. There were seven significant earthquakes with magnitude ≥ 5,0. The majority (85%) of earthquakes were shallow (< 30 km) and 56% had a low magnitude (Mw 3,0-3,9). Local and regional faulting caused 52% of the felt earthquakes and 45% occurred due to the subduction of the Cocos Plate beneath the Caribbean Plate and the Panama microplate. The highest intensity observed during 2013 was VI (Modified Mercalli, MM) in the Sixaola region (Limon) during the May 27 earthquake (5.6 Mw) with epicenter in western Panama

https://doi.org/10.15517/rgac.v51i1.17043
PDF (Español (España))

References

ADAMEK, S., FROHLICH, C. & PENNINGTON, W., 1988: Seismicity of the Caribbean-Nazca Boundary Constraints on Microplate Tectonics of the Panama Region.- J. Geophys. Res. 93: 2053-2075.

LIENERT, B. R. & HAVSKOV, J., 1995: A computer program for locating earthquakes both locally and globally.- Seis. Res. Lett. 66: 26-36, DOI: 10.1785/gssrl.66.5.26

MARSHALL, J. S., FISHER, D. M. & GARDNER, T. W., 2000: Central Costa Rica deformed belt: Kinematics of diffuse faulting across the western Panama block.- Tectonics, 19: 468-492.

OTTEMÖLLER, L., VOSS, P. & HAVSKOV, J., 2011: SEISAN: Tthe earthquake analysis software for Windows, Solaris, LINUX, and MACOSX, version 9.0.1.- 361 págs. Univ. of Bergen, Bergen.

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