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Carnegie Ridge
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information
Tectonic Segmentation of the North Andean Margin: Impact of the Carnegie Ridge Collision
Revised Tectonic Boundaries in the Cocos Plate Off Costa Rica Implications for the Segmentation of the Convergent Margin And
Tectonic Evolution of the Andes of Ecuador, Peru, Bolivia and Northern
Impact of the Carnegie Ridge Collision
Young Tracks of Hotspots and Current Plate Velocities
Geothermal Country Update for Ecuador, 2000-2005
A Plate Model for Jurassic to Recent Intraplate Volcanism in the Pacific Ocean Basin
Technical Memorandum 86160 ANDEAN TECTONICS
Tectonic Assembly of the Northern Andean Block, in C
Program and Abstracts Red.Pdf
Geochemical and Isotopic Variations in a Frontal Arc Volcanic Cluster (Chachimbiro-Pulumbura-Pilavo-Yanaurcu, Ecuador)
An Overview of the Main Quaternary Deformation of South America
Open-Source Archive of Active Faults for Northwest South America
1 Horizontal Subduction Zones, Convergence Velocity And
Effects of Oceanic Crustal Thickness on Intermediate Depth Seismicity
Structure and Tectonic History of the Eastern Panama Basin
7. Plate Tectonic Evolution of the Cocos-Nazca Spreading Center1
Top View
An Interplay Between Subduction Dynamics and Crustal Wedge Tectonics Joseph Martinod, Mélanie Gérault, Laurent Husson, Vincent Regard
Tectonic Segmentation of the North Andean Margin: Impact of the Carnegie Ridge Collision
Regional Geology of Ecuador
Seismic Structure of the Carnegie Ridge and the Nature of the Galapagos´ Hotspot ∗ Valent´I Sallar`Es1, Philippe Charvis,1 Ernst R
Redalyc.Arguments for and Against the Pacific Origin of the Caribbean Plate: Discussion, Finding for an Inter-American Origin
Sediment Distribution and Depositional Processes On
The Romeral Fault (Copia).Indd
Geochemical and Isotopic Characterization of Volcanic and Geothermal Fluids Discharged from the Ecuadorian Volcanic
PDF Linkchapter
Subduction Consequences Along the Andean Margin: Thermal and Topographic Signature of an Ancient Ridge Subduction in the Marañón Basin of Perú