Quantitative Relationships Between Basalt Geochemistry, Shear Wave Velocity, and Asthenospheric Temperature Beneath Western North America

Author:

Klöcking M.1ORCID,White N. J.1ORCID,Maclennan J.1ORCID,McKenzie D.1,Fitton J. G.2ORCID

Affiliation:

1. Bullard Laboratories, Department of Earth Sciences; University of Cambridge; Cambridge UK

2. Grant Institute, School of GeoSciences; University of Edinburgh; Edinburgh UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference135 articles.

1. 3-D multiobservable probabilistic inversion for the compositional and thermal structure of the lithosphere and upper mantle: III. Thermochemical tomography in the Western-Central U.S.;Afonso;Journal of Geophysical Research: Solid Earth,2016

2. Gravity, bathymetry and convection in the Earth;Anderson;Earth and Planetary Science Letters,1973

3. African lithospheric structure, volcanism, and topography;Ashwal;Earth and Planetary Science Letters,1989

4. Intraplate volcanism at the edges of the Colorado Plateau sustained by a combination of triggered edge-driven convection and shear-driven upwelling;Ballmer;Geochemistry, Geophysics, Geosystems,2015

5. Static and dynamic support of western United States topography;Becker;Earth and Planetary Science Letters,2013

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