Monitoring Nuclear Tests-Reference-Cited by-同舟云学术

Monitoring Nuclear Tests

Published:1998-09-25 Issue:5385 Volume:281 Page:1967-1968
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Barker Brian¹,Clark Michael²,Davis Peter³,Fisk Mark⁴,Hedlin Michael³,Israelsson Hans²,Khalturin Vitaly⁵,Kim Won-Young⁵,McLaughlin Keith²,Meade Charles⁶,North Robert²,Orcutt John³,Powell Chris⁷,Richards Paul G.⁵,Stead Richard²,Stevens Jeffry¹,Vernon Frank³,Murphy John¹,Wallace Terry⁸

Affiliation:

1. Maxwell Technologies, Reston, VA 22091, USA.

2. Center for Monitoring Research, Science Application International Corporation, Arlington, VA 22209, USA.

3. Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92037, USA.

4. Mission Research Corporation, Newington, VA 22122, USA.

5. Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA.

6. RAND Corporation, 1333 H Street, N.W., Washington, DC 20005, USA.

7. Autometric, Alexandria, VA 22312, USA.

8. Department of Geosciences, University of Arizona, Tucson, AZ 85745, USA.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference15 articles.

1. The text of the CTBT specifies the locations and characteristics of the IMS stations. It includes a primary network of 50 seismic stations and an auxiliary network of 120 stations 80 radionuclide detectors 11 hydroacoustic stations and 60 infrasound stations.

2. Thirty-six primary and 58 auxiliary seismic stations are now operational. In its current state the network relies on voluntary efforts and contributions of national governments and organizations. In the future six of the primary stations will be upgraded from single three-component sensors to multistation arrays. All stations will be linked by satellite directly to the IDC.

3. Details of the results can be found at the PIDC Web page (http://www.pidc.org/dataprodbox/prod.html).

4. Historically the most reliable screen has been the difference between long-period surface ( M s) and short-period body ( m b) wave magnitudes. For explosions m b is typically greater than (1.76 + 0.8 M s). Spectral ratios of regional P S waves tend to separate earthquake and explosion populations because of differences in the compressional and shear wave energy emitted by explosive and earthquake sources.

5. The PIDC uses IASPEI-91 for all seismic locations except in the Baltic shield where a specially calibrated model has been implemented.

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