Instituto Geológico y Minero de España

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Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 10 de 13 encontrados

1.-  Along-strike variability of coupled hinterland-foreland processes during formation of the Magallanes foreland basin, Patagonian Andes
Geological Society of America (GSA); Boulder, CO; USA; United States, 2011
Geological Society of America, 2011 annual meeting
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2.-  ASSESSING THE CONSEQUENCES OF RIDGE COLLISION, OBLIQUE SUBDUCTION AND ARC-PARALLEL STRIKE-SLIP FAULTING IN THE SOUTHERN CHILEAN ANDES (44 DEGREES TO 48 DEGREES S) USING FISSION TRACK DATA
CAMBRIDGE PUBLICATIONS; CAMBRIDGE; GBR; UNITED KINGDOM, 1999
EUROPEAN UNION OF GEOSCIENCES CONFERENCE; EUG 10; ABSTRACTS
Ver registro

3.-  FISSION TRACK THERMOCHRONOLOGY OF THE SOUTHERN CHILEAN ANDES IN THE REGION OF THE CHILE TRIPLE JUNCTION AND LIQUINE-OFQUI FAULT ZONE (42 DEGREES TO 48 DEGREES S); A PRELIMINARY REPORT
SOCIETA COOPERATIVA TIPOGRAFICA; PADUA; ITA; ITALY, 1999
FISSION TRACK ANALYSIS; THEORY AND APPLICATIONS
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4.-  Glacial control on active mountain development; a southward latitudinal transition from glacial buzzsaw to glacial shield in the Patagonian Andes
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2008
European Geosciences Union general assembly 2008
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5.-  Glaciation as a destructive and constructive control on mountain building
Macmillan Journals; London; GBR; United Kingdom, 2010
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6.-  LATE CENOZOIC GEOMORPHIC AND TECTONIC EVOLUTION OF THE PATAGONIAN ANDES BETWEEN LATITUDES 42 DEGREES S AND 46 DEGREES S; AN APPRAISAL BASED ON FISSION-TRACK RESULTS FROM THE TRANSPRESSIONAL INTRA-ARC LIQUINE-OFQUI FAULT ZONE
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2002
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7.-  MESOZOIC-CENOZOIC DENUDATION HISTORY OF THE PATAGONIAN ANDES (SOUTHERN CHILE) AND ITS CORRELATION TO DIFFERENT SUBDUCTION PROCESSES
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2001
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8.-  P-T evolution and timing of a late Palaeozoic fore-arc system and its heterogeneous Mesozoic overprint in north-central Chile (latitudes 31-32 degrees S)
Cambridge University Press; London; GBR; United Kingdom, 2012
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9.-  The geodynamics of collision of a microplate (Chilenia) in Devonian times deduced by the pressure-temperature-time evolution within part of a collisional belt (Guarguaraz Complex, W Argentina)
Springer International; Heidelberg - New York; III; International, 2011
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10.-  THE GEOMORPHIC AND TECTONIC RESPONSE OF THE UPPER PLATE TO DIFFERENT SUBDUCTION PROCESSES ASSESSED USING FISSION TRACK THERMOCHRONOLOGY; AN EXAMPLE FROM THE SOUTHERN CHILEAN ANDES
DEUTSCHE GEOLOGISCHE GESELLSCHAFT; HANOVER; DEU; FEDERAL REPUBLIC OF GERMANY, 2001
2001 MARGINS MEETING; INTERNATIONAL CONFERENCE AND ANNUAL MEETING OF THE DEUTSCHE GEOLOGISCHE GESELLSCHAFT AND GEOLOGISCHE VEREINIGUNG; PROGRAM AND ABSTRACTS
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