Registros del 1 al 10 de 19 encontrados |
![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 5.- Damage surrounding dynamically propagating shear cracks in granodiorite
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
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![](./images/clear.gif) 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)
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![](./images/clear.gif) 7.- Fault zone structure and evolution at continental plate boundaries
2011
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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![](./images/clear.gif) 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
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