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Earthquake Magnitude Measurements for Puerto Rico

¹ Department of Earth Science
Carleton University
Ottawa, Ontario, K1S5B6
gma{at}ccs.carleton.ca
dariush{at}ccs.carleton.ca

Reliable determination of earthquake magnitude is a fundamental building block of seismic hazard assessment. The seismicity catalog for Puerto Rico is dominated by small earthquakes (M < 5), mostly M_D (a local magnitude based on duration) and m_b (body-wave magnitude). There is considerable uncertainty over the interpretation of M_D. To reduce this uncertainty, we evaluate moment magnitude (M) and M₁ (1-Hz magnitude) for events within the catalog and develop relationships between these and other magnitude measures.

The available seismographic data are mostly short-period records, because broadband instruments in Puerto Rico have been installed only recently. A difficulty with the calculation of moment magnitude is that short-period data do not generally extend to sufficiently low frequencies to reliably obtain the displacement spectrum at low frequencies. Moment magnitudes for small earthquakes in Puerto Rico are thus estimated from a single broadband station and subject to much uncertainty. To get around this difficulty, we used M₁, which closely tracks moment magnitude for small to moderate events (Chen and Atkinson, 2002). M₁ is obtained from the spectral amplitude at 1 Hz and is defined such that it will equal moment magnitude for earthquakes following a Brune point-source model. Unlike moment magnitude, M₁ can be determined from short-period seismograms. Our values of M and M₁ are in close agreement with each other for small to moderate earthquakes. There is a systematic difference between M₁ or M and catalog magnitudes m_b or M_D, with the catalog magnitude exceeding moment magnitude by about 0.4 units on average. It is recommended that M₁ be used as a regional magnitude scale for earthquakes in Puerto Rico, and as an estimate of M for events of M < 5.

Online material: List of earthquakes in Puerto Rico from 1993 through 2002.