Registros del 1 al 10 de 113 encontrados |
1.- A preliminary receiver function investigation of the crustal structure in the Iberia-Africa plate boundary Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2008 European Geosciences Union general assembly 2008 Ver registro
2.- A receiver function study of the Central America and Cascadia subduction zone systems 2009 Ver registro
3.- A receiver function study of the southern Costa Rican subduction zone Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2008 European Geosciences Union general assembly 2008 Ver registro
4.- A search for Sp converted phase in MASE seismic data from the steeply dipping slab beneath central Mexico American Geophysical Union; Washington, DC; USA; United States, 2008 AGU 2008 fall meeting Ver registro
5.- An investigation into crustal structure of South America; the continent that is missing some of its Moho American Geophysical Union; Washington, DC; USA; United States, 2003 AGU 2003 fall meeting Ver registro
6.- An investigation of crust and upper mantle structure in western Argentina utilizing local event receiver functions American Geophysical Union; Washington, DC; USA; United States, 2004 AGU 2004 fall meeting Ver registro
7.- An investigation of lithospheric structure and evolution in convergent orogenic systems using seismic receiver functions and surface wave analysis 2008 Ver registro
8.- Basement depths in the Parecis Basin (Amazon) with receiver functions from small local earthquakes in the Porto dos Gauchos seismic zone Elsevier; Oxford; GBR; United Kingdom, 2011 Ver registro
9.- Broadband seismological imaging of flat-slab subduction and its long-term impact on lithospheric structure and processes 2011 Ver registro
10.- COMBINED RECEIVER-FUNCTION AND SURFACE WAVE PHASE-VELOCITY INVERSION USING A NICHING GENETIC ALGORITHM; APPLICATION TO PATAGONIA SEISMOLOGICAL SOCIETY OF AMERICA; BERKELEY, CA; USA; UNITED STATES, 2004 Ver registro
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