Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95407/1/jgrb15974.pd
Determining the scale-length, magnitude, and distribution of heterogeneity in the lowermost mantle i...
[1] We measure seismic attenuation beneath North America using waveform cross-correlation and cluste...
When an earthquake ruptures, seismic waves propagate through the Earth. We can utilise information f...
[1] We estimate the spatial variation of the seismic parameter t * using teleseismic (epicentral dis...
Using Mw>6, deep earthquakes that occurred between 2006 and 2015 and were recorded by EarthScope’s T...
The latest results concerning the depth variation of Q, P- and S-wave velocities obtained by various...
Both spectral and time domain studies indicate that the frequency dependence and regional variation ...
In a study of variation of the compressional velocity with depth in the C region of the upper mantle...
Using available digital seismic stations deployed since the 1980’s, the largest data set based on br...
From the reprocessed data set of Engdahl and co-workers we have carefully selected matching P and S ...
Thesis: Ph. D. in Geophysics, Massachusetts Institute of Technology, Department of Earth, Atmospheri...
dT/dA and azimuth measurements at the Yellowknife Seismic Array (YKA) for P and pP phases that have ...
We simultaneously invert for the velocity and attenuation structure of the North American mantle fro...
International audienceMapping variations in the attenuation of seismic energy is important for under...
The unique physical and chemical properties of cratonic lithosphere are thought to be key to its lon...
Determining the scale-length, magnitude, and distribution of heterogeneity in the lowermost mantle i...
[1] We measure seismic attenuation beneath North America using waveform cross-correlation and cluste...
When an earthquake ruptures, seismic waves propagate through the Earth. We can utilise information f...
[1] We estimate the spatial variation of the seismic parameter t * using teleseismic (epicentral dis...
Using Mw>6, deep earthquakes that occurred between 2006 and 2015 and were recorded by EarthScope’s T...
The latest results concerning the depth variation of Q, P- and S-wave velocities obtained by various...
Both spectral and time domain studies indicate that the frequency dependence and regional variation ...
In a study of variation of the compressional velocity with depth in the C region of the upper mantle...
Using available digital seismic stations deployed since the 1980’s, the largest data set based on br...
From the reprocessed data set of Engdahl and co-workers we have carefully selected matching P and S ...
Thesis: Ph. D. in Geophysics, Massachusetts Institute of Technology, Department of Earth, Atmospheri...
dT/dA and azimuth measurements at the Yellowknife Seismic Array (YKA) for P and pP phases that have ...
We simultaneously invert for the velocity and attenuation structure of the North American mantle fro...
International audienceMapping variations in the attenuation of seismic energy is important for under...
The unique physical and chemical properties of cratonic lithosphere are thought to be key to its lon...
Determining the scale-length, magnitude, and distribution of heterogeneity in the lowermost mantle i...
[1] We measure seismic attenuation beneath North America using waveform cross-correlation and cluste...
When an earthquake ruptures, seismic waves propagate through the Earth. We can utilise information f...
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