Seismic High Attenuation Region Observed Beneath Southern New England From Teleseismic Body Wave Spectra: Evidence for High Asthenospheric Temperature Without Melt-Reference-Cited by-同舟云学术

Seismic High Attenuation Region Observed Beneath Southern New England From Teleseismic Body Wave Spectra: Evidence for High Asthenospheric Temperature Without Melt

Published:2017-11-11 Issue:21 Volume:44 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Dong Mingduo T.¹²^ORCID,Menke William H.¹²^ORCID

Affiliation:

1. Lamont‐Doherty Earth Observatory Palisades NY USA

2. Department of Earth and Environmental Science Columbia University New York NY USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL074953

Reference78 articles.

1. Reconciling mantle attenuation-temperature relationships from seismology, petrology, and laboratory measurements

2. Scaling law of seismic spectrum

3. Earthquake Ground-Motion Prediction Equations for Eastern North America

4. Effects of elastic focusing on global models of Rayleigh wave attenuation

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