Registros del 1 al 10 de 41 encontrados |
1.- 1, SEISMOLOGICAL OBSERVATIONS OF UPPER MANTLE ANISOTROPY; 2, SOURCE SPECTRA OF SHALLOW SUBDUCTION ZONE EARTHQUAKES AND THEIR TSUNAMIGENIC POTENTIAL 1999 Ver registro
2.- Anisotropy and mantle flow in the eastern Sierras Pampeanas from shear wave splitting American Geophysical Union; Washington, DC; USA; United States, 2009 AGU 2009 fall meeting Ver registro
3.- Anisotropy in the Chile-Argentina flat slab subduction zone, South America American Geophysical Union; Washington, DC; USA; United States, 2003 AGU 2003 fall meeting Ver registro
4.- Combining the evidence; crustal and upper mantle structure above the flat slab in central Chile and Argentina American Geophysical Union; Washington, DC; USA; United States, 2006 AGU 2006 fall meeting Ver registro
5.- Complex anisotropy beneath the Peruvian flat slab from frequency-dependent, multiple-phase shear wave splitting analysis Wiley-Blackwell for American Geophysical Union; Washington, DC; USA; United States, 2013 Ver registro
6.- Constraints on mantle flow at the Caribbean-South American plate boundary inferred from shear wave splitting American Geophysical Union; Washington, DC; USA; United States, 2009 Ver registro
7.- Corner flow in the Isthmus of Tehuantepec, Mexico inferred from anisotropy measurements using local intraslab earthquakes Oxford University Press on behalf of The Royal Astronomical Society, the Deutsche Geophysikalische G, 2013 Ver registro
8.- Crust and upper mantle structure in central Brazil derived by receiver functions and SKS splitting analysis Elsevier; Oxford; GBR; United Kingdom, 2012 mplete Ver registro
9.- CRUSTAL AND UPPER MANTLE STRUCTURE IN THE AMAZON REGION (BRAZIL) DETERMINED WITH BROADBAND MOBILE STATIONS AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002 Ver registro
10.- Deep deformation pattern from electrical anisotropy in an arched orogen (Betic Cordillera, western Mediterranean) Geological Society of America (GSA); Boulder, CO; USA; United States, 2010 Ver registro
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