Frequency-magnitude statistics and spatial correlation dimensions of earthquakes at Long Valley caldera, California

Details Frequency-magnitude statistics and spatial correlation dimensions of earthquakes at Long Valley caldera, California Frequency-magnitude statistics and spatial correlation dimensions of earthquakes at Long Valley caldera, California

Aug 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999geoji.138..563b&link_type=abstract

Geophysical Journal International, Volume 138, Issue 2, pp. 563-570.

Astronomy and Astrophysics

Astronomy

5

Earthquakes, Fractal, Long Valley

Scientific paper

Intense earthquake swarms at Long Valley caldera in late 1997 and early 1998 occurred on two contrasting structures. The first is defined by the intersection of a north-northwesterly array of faults with the southern margin of the resurgent dome, and is a zone of hydrothermal upwelling. Seismic activity there was characterized by high b-values and relatively low values of D, the spatial fractal dimension of hypocentres. The second structure is the pre-existing South Moat fault, which has generated large-magnitude seismic activity in the past. Seismicity on this structure was characterized by low b-values and relatively high D. These observations are consistent with low-magnitude, clustered earthquakes on the first structure, and higher-magnitude, diffuse earthquakes on the second structure. The first structure is probably an immature fault zone, fractured on a small scale and lacking a well-developed fault plane. The second zone represents a mature fault with an extensive, coherent fault plane.

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