| Registros del 1 al 10 de 18 encontrados |
1.- (SUPER 186) OS- (SUPER 187) OS SYSTEMATICS OF GORGONA KOMATIITES AND ICELAND PICRITES
PERGAMON; OXFORD; III; INTERNATIONAL, 2002
ABSTRACTS OF THE 12TH ANNUAL V. M. GOLDSCHMIDT CONFERENCE
Ver registro
2.- A BROADBAND SEISMIC STUDY OF THE LOWERMOST MANTLE BENEATH MEXICO; CONSTRAINTS ON ULTRALOW VELOCITY ZONE ELASTICITY AND DENSITY
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2001
Ver registro
3.- A BROADBAND SEISMIC STUDY OF THE LOWERMOST MANTLE BENEATH MEXICO; FURTHER EVIDENCE OF A PARTIAL MELT ORIGIN OF ULTRALOW VELOCITY ZONES
SEISMOLOGICAL SOCIETY OF AMERICA, EASTERN SECTION; [BERKELEY, CA]; USA; UNITED STATES, 1999
SSA-99 94TH ANNUAL MEETING; MEETING ABSTRACTS
Ver registro
4.- A model for the large-scale evolution of mantle structure, surface and core-mantle boundary heat fluxes and surface vertical motions since the early Paleozoic
2011
Ver registro
5.- ABSENCE OF SHORT-PERIOD ULVZ PRECURSORS TO PCP AND SCP FROM TWO REGIONS OF THE CMB
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2001
Ver registro
6.- Bulldozing the core-mantle boundary; localized seismic scatterers beneath the Caribbean Sea
Elsevier; Amsterdam; NLD; Netherlands, 2008
Ver registro
7.- EVIDENCE FOR AN S VELOCITY DISCONTINUITY IN THE LOWERMOST MANTLE BENEATH THE SOUTHEASTERN PACIFIC BASIN
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1997
Ver registro
8.- EXTREMELY LARGE AMPLITUDE SCP PHASES; A UNIQUE SPOT ON THE CMB
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1999
AGU 1999 FALL MEETING
Ver registro
9.- GEOMAGNETISMO JURASICO, ZONAS DE SUBDUCCION DE PANGEA Y ANOMALIAS EN LA VELOCIDAD DE ONDAS SISMICAS EN EL LIMITE MANTO-NUCLEO
2005
Ver registro
10.- Impingement of deep mantle-derived upwelling beneath northern, subducted extension of the East Pacific Rise and palinspastically restored Cenozoic mafic magmatism in western North America
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
Ver registro
|
|
|
