thumbnail

The P-wave velocity of the uppermost mantle of the Rio Grande rift region of north central New Mexico.

Journal of Geophysical Research

By:
and

Links

  • The Publications Warehouse does not have links to digital versions of this publication at this time
  • Download citation as: RIS

Abstract

A network of seismograph stations has operated in north-central New Mexico since 1975. The network is approximately 200 by 300 km in size and encompasses the Rio Grande rift there. Several seismic refraction experiments have been reported in the literature for the region of the network and adjacent areas. Because all of the seismic refraction lines are unreversed, Pn velocities reported were mainly of the inverse travel time slope for the direction of the corresponding line. The values of the inverse slope for those studies range from 7.6 to 8.2 km/s. The purpose of our study is to estimate the P-wave velocity of the uppermost mantle by using the time term method. First, we timed the Pn waves of strong signals from five explosions and eight shallow earthquakes recorded by the network. The main data set, which contains 87 time-distance pairs, was processed by using the time term method. The Pn velocity estimated by this method is 8.0 + or - 0.1 km/s. To corroborate this estimate, we then processed 10 subsets of the main data set in the same way. Almost all of the solutions show velocities of 7.9-8.1 km/s, in agreement with the velocity determined for the main data set. -Authors

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
The P-wave velocity of the uppermost mantle of the Rio Grande rift region of north central New Mexico.
Series title:
Journal of Geophysical Research
Volume
86
Issue:
B8
Year Published:
1981
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Journal of Geophysical Research
First page:
7055
Last page:
7063