Crustal Shear Wave Velocity Structure of Central Idaho and Eastern Oregon From Ambient Seismic Noise: Results From the IDOR Project

Author:

Bremner Paul M.1ORCID,Panning Mark P.12ORCID,Russo R. M.1ORCID,Mocanu Victor3,Stanciu A. Christian14ORCID,Torpey Megan15,Hongsresawat Sutatcha16,VanDecar John C.7ORCID,LaMaskin Todd A.8,Foster D. A.1ORCID

Affiliation:

1. Department of Geological Sciences University of Florida Gainesville FL USA

2. Now at Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA

3. Department of Geology and Geophysics University of Bucharest Bucharest Romania

4. Now at Earth Sciences Department University of Oregon Eugene OR USA

5. Now at AIR Worldwide Boston MA USA

6. Now at Division of Geoscience, Mahidol University Kanchanaburi Thailand

7. DTM‐Carnegie Institution of Washington Washington DC USA

8. Department of Geography and Geology University of North Carolina at Wilmington Wilmington NC USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference88 articles.

1. Evolving geographic patterns of Cenozoic magmatism in the North American Cordillera: The temporal and spatial association of magmatism and metamorphic core complexes

2. Petrology and deformation history of the burnt river schist and associated plutonic rocks in the burnt river canyon area, northeastern Oregon;Ashley R.;Geology of the Blue Mountains region of Oregon, Idaho, and Washington: Petrology and tectonic evolution of pre‐Tertiary rocks of the Blue Mountains region: US Geological Survey Professional Paper,1995

3. Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements

4. Breakup of a supercontinent between 625 Ma and 555 Ma: new evidence and implications for continental histories

5. Pn tomography of the western United States using USArray

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