Shear wave velocities and crustal structure of the Eastern Snake River Plain, Idaho
- 10 April 1982
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 87 (B4), 2643-2653
- https://doi.org/10.1029/jb087ib04p02643
Abstract
No abstract availableThis publication has 27 references indexed in Scilit:
- The nature of the lower continental crust: Inferences from geophysics, surface geology, and crustal xenolithsReviews of Geophysics, 1981
- Velocity and attenuation in partially molten rocksJournal of Geophysical Research, 1980
- Regional S-wave structure for southern California from the analysis of teleseismic Rayleigh wavesGeophysical Journal International, 1979
- Deep structure under Yellowstone National Park U.S.A.: A continental “hot spot”Tectonophysics, 1979
- Surface waves and the structure of the Great Basin of Nevada and western UtahJournal of Geophysical Research, 1978
- The effect of high temperature and high confining pressure on compressional wave velocities in quartz-bearing and quartz-free igneous and metamorphic rocksTectonophysics, 1978
- K-Ar dating, Quaternary and Neogene volcanic rocks of the Snake River Plain, IdahoAmerican Journal of Science, 1975
- Constitution of the Lower Continental Crust Based on Experimental Studies of Seismic Velocities in GranuliteGSA Bulletin, 1975
- A Discussion on volcanism and the structure of the Earth - Cenozoic volcanism and plate-tectonic evolution of the Western United States. II. Late cenozoicPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1972
- An Algorithm for Least-Squares Estimation of Nonlinear ParametersJournal of the Society for Industrial and Applied Mathematics, 1963