Frequency-magnitude distribution of microearthquakes beneath the 9°50′N region of the East Pacific Rise, October 2003 through April 2004

Author:

Bohnenstiehl D. R.1,Waldhauser F.2,Tolstoy M.2

Affiliation:

1. Department of Marine, Earth and Atmospheric Sciences; North Carolina State University; Campus Box 8208,; Raleigh; North Carolina; 27695; USA

2. Lamont-Doherty Earth Observatory of Columbia University; P.O. Box 1000,; Palisades; New York; 10964; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference76 articles.

1. Maximum likelihood estimate of b in the formula log n = a−bm and its confidence limits;Aki;Bull. Earthquake Res. Inst. Tokyo,1965

2. Brittle-ductile transition and associated seismicity; experimental and numerical studies and relationship with the b value;Amitrano;J. Geophys. Res.,2003

3. The ML scale in central California;Bakun;Bull. Seismol. Soc. Am.,1984

4. Microearthquake characteristics and crustal Vp − Vs structure at the Mid-Atlantic Ridge, 35°N;Barclay;J. Geophys. Res.,2001

5. Frequency-magnitude statistics and spatial correlation dimensions of earthquakes at Long Valley Caldera, California;Barton;Geophys. J. Int.,1999

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