Registros del 1 al 10 de 22 encontrados |
1.- A RARE OBSERVATION OF "NEAR-FIELD" AND S660P FROM A SINGLE BROADBAND SEISMOGRAM RECORDED IN CALIFORNIA FOR A DEEP EARTHQUAKE NEAR BONIN AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2000 AGU 2000 FALL MEETING Ver registro
2.- CONSTRAINTS ON FLOW IN THE MANTLE FROM A NEW DEGREE-20 SHEAR VELOCITY MODEL AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1999 AGU 1999 FALL MEETING Ver registro
3.- Evidence for deep mantle convection and primordial heterogeneity from nitrogen and carbon stable isotopes in diamond Elsevier; Amsterdam; NLD; Netherlands, 2012 Ver registro
4.- Evidence of a mid-mantle discontinuity beneath South America American Geophysical Union; Washington, DC; USA; United States, 2006 AGU 2006 fall meeting Ver registro
5.- Frequency-dependent phase coherence for noise suppression in seismic array data American Geophysical Union; Washington, DC; USA; United States, 2007 Ver registro
6.- Global mantle convection; evidence from carbon and nitrogen isotopes in super-deep diamonds American Geophysical Union; Washington, DC; USA; United States, 2009 AGU 2009 fall meeting Ver registro
7.- Imaging the mantle transition zone beneath the South American platform using P- and S-wave receiver functions Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Federal R, 2009 European Geosciences Union general assembly 2009 Ver registro
8.- Large exchange through the 660 km discontinuity; evidence from C- and N-isotopes in super-deep diamonds Elsevier; New York, NY; III; International, 2010 Abstracts of the 20th annual V. M. Goldschmidt conference Ver registro
9.- Mantle transition zone beneath the Caribbean-South American plate boundary and its tectonic implications Elsevier; Amsterdam; NLD; Netherlands, 2010 Ver registro
10.- MINERAL INCLUSIONS IN DIAMONDS; ASSOCIATIONS AND CHEMICAL DISTINCTIONS AROUND THE 670-KM DISCONTINUITY SPRINGER INTERNATIONAL; HEIDELBERG-NEW YORK; III; INTERNATIONAL, 2001 Ver registro
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