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Title: Velocity structure of the Long Valley caldera from the inversion of local earthquake P and S travel times

Journal Article · · Journal of Geophysical Research
DOI:https://doi.org/10.1029/93JB01553· OSTI ID:67926
; ;  [1]
  1. Lawrence Berkeley Lab., CA (United States)

A high-resolution tomographic study of the Long Valley region began in 1989 with the installation of a special fan array of eight three-component borehole (80-160 m depths) receivers on the northwestern rim of the caldera to provide the data necessary for a joint inversion for hypocenters and the three-dimensional P and S wave velocity structure in and below the caldera. The experiment specifically targeted the subsurface location of the previously inferred magma chamber beneath the Resurgent Dome. Additional coverage was provided by existing US Geological Survey and University of Nevada, Reno seismographic networks. The authors employed the progressive inversion scheme of Thurber, with cubic spline interpolation after Michelini and McEvilly. The final model is based on data from 280 well-distributed local earthquakes. Some 6900 arrival times were used, including about 700 S wave times from the three-component stations. The resulting velocity structure reflects the known geology, defining the low-velocity Sierran block and highland terrane. No isolated distinct low-velocity anomalies are revealed beneath the caldera floor, although a diffuse zone of reduced velocity persists to a depth of about 8 km. These lower velocities may be related to hydrothermal alteration and/or extensive fractures. The Vp/Vs structure contains significant lateral variation within and beneath the caldera to about 8 km depth, and these variations can be related to accepted models of the active geothermal system. The lack of a significant S wave velocity anomaly, along with the normal or low values of the Vp/Vs ratio, argues against the presence of a sizable and distinct magma body at shallow to midcrustal depth beneath Long Valley caldera, although a very low percentage of partial melt cannot be precluded. 37 refs., 7 figs.

Sponsoring Organization:
USDOE
DOE Contract Number:
AC03-76SF00098
OSTI ID:
67926
Journal Information:
Journal of Geophysical Research, Vol. 98, Issue B11; Other Information: PBD: 10 Nov 1993
Country of Publication:
United States
Language:
English

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