Instituto Geológico y Minero de España

LogoSistema de información documental - SID

 

 

 

Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 10 de 19 encontrados

1.-  A melt origin for spinifex-textured metaperidotite in the Cerro del Almirez Massif, southern Spain
Yale University, Kline Geology Laboratory; New Haven, CT; USA; United States, 2012
Ver registro

2.-  An integrated magnetic and geological study of cataclasite-dominated pseudotachylytes in the Chiapas Massif, Mexico; a snapshot of stress orientation following slip
Blackwell Science for the Royal Astronomical Society, the Deutsche Geophysikalische Gesellschaft and, 2009
Ver registro

3.-  Anatomy of an ancient subduction channel in the depth range of its seismogenic coupling zone; insights from field studies in the Swiss Alps and southern Chile
GeoForschungsZentrum Potsdam; Potsdam; DEU; Federal Republic of Germany, 2008
Ver registro

4.-  APPARENT TRUNCATION AND JUXTAPOSITION OF CAMBRIAN AND ORDOVICIAN ARC-ACCRETIONARY COMPLEXES, EASTERN SIERRAS PAMPEANAS, ARGENTINA
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2001
GEOLOGICAL SOCIETY OF AMERICA, 2001 ANNUAL MEETING
Ver registro

5.-  Damage surrounding dynamically propagating shear cracks in granodiorite
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
Ver registro

6.-  Dating fault fabrics using modern techniques of (super 40) Ar/ (super 39) Ar thermochronology; evidence for Paleozoic deformation in the eastern Sierras Pampeanas, Argentina
Australian Crustal Research Centre, Monash University; Clayton, Victoria; AUS; Australia, 2008
Making sense of shear (in honour of Carol Simpson)
Ver registro

7.-  Fault zone structure and evolution at continental plate boundaries
2011
Ver registro

8.-  Geochronological constraints on the age of a Permo-Triassic impact event; U/Pb and (super 40) Ar/ (super 39) Ar results for the 40 km Araguainha Structure of central Brazil
Elsevier; New York, NY; III; International, 2012
Ver registro

9.-  HIGH STRAIN-RATE DEFORMATION FABRICS CHARACTERIZE A KILOMETERS-THICK PALEOZOIC FAULT ZONE IN THE EASTERN SIERRAS PAMPEANAS, CENTRAL ARGENTINA
PERGAMON; OXFORD; III; INTERNATIONAL, 2003
Ver registro

10.-  HIGH TEMPERATURE, HIGH STRAIN-RATE FABRICS DEFINE A MAJOR DUCTILE SHEAR ZONE IN THE EASTERN SIERRAS PAMPEANAS, ARGENTINA
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2001
GEOLOGICAL SOCIETY OF AMERICA, 2001 ANNUAL MEETING
Ver registro


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