New Mexico Geological Society Annual Spring Meeting — Abstracts
Seismic wave attenuation in the upper crust of the Rio Grande rift near Socorro, New Mexico
Philip J. Carpenter1 and Allan R. Sanford1
Spectra from over 400 digitally rec orded microearthquakes in the magnitude range -0.8 to 1.2 were used to compute apparent seismic quality factors (Q) for upper crustal rocks (0-19 km) within 45 km of Socorro. In this study apparent Q is a measure of seismic wave attenuation due to intrinsic absorption and scattering. It was found that:
(1) Relatively low Qp and Qs regions exist at depths of 7-10 km beneath Socorro Peak and the southwestern part of the La Jencia basin. These relatively low Q regions may result from small magmatic intrus ions or a high density of fluid-filled fractures at depth.
(2) Near-surface low Q regions have a profound effect on apparent Qp or Qs measured at the surface. Near-surface low Q regions vary from 0.3-2 km in thickness and exhibit Q values less than 50, and often less than 10.
(3) Qp/Qs varies from less than 0.5 to about 1.0. The observed Qp/Qs depends on the event distance.
(4) The average Qs for the upper crust in the central Rio Grande rift, excludin g the near-sur face low Q layer, is greater than 500.
1984 New Mexico Geological Society Annual Spring Meeting
April 27, 1984, Macey Center
Online ISSN: 2834-5800