Registros del 1 al 5 de 5 encontrados |
![](./images/clear.gif) 1.- EROSIVE AND ACCRETIVE MASS TRANSFER MODES AND DEFORMATION AT THE CHILEAN FOREARC; RESULTS OF 2D SCALED SANDBOX EXPERIMENTS
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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![](./images/clear.gif) 2.- Exhumation by basal accretion; insights from combined isotope tectonochronology and sandbox modelling of the south-central Chilean accretionary wedge
[International Geological Congress]; [location varies]; III; International, 2004
Italia 2004; 32nd international geological congress; abstracts
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![](./images/clear.gif) 3.- Long-term geological evolution and mass-flow balance of the south-central Andes
Springer; Berlin; DEU; Federal Republic of Germany, 2006
The Andes; active subduction orogeny
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![](./images/clear.gif) 4.- MECHANICS AND MASS TRANSFER PATTERNS OF TECTONIC EROSIVE CONVERGENT MARGINS; QUANTITATIVE RESULTS FROM ANALOGUE SANDBOX MODELS AND THEIR IMPLICATIONS FOR NATURAL FOREARC SYSTEMS
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2000
AGU 2000 FALL MEETING
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![](./images/clear.gif) 5.- Subduction channel evolution in brittle fore-arc wedges; a combined study with scaled sandbox experiments, seismological and reflection seismic data and geological field evidence
Springer; Berlin; DEU; Federal Republic of Germany, 2006
The Andes; active subduction orogeny
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