A5080400237- Geological and Tectonic Studies in Latin America
- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Geological formations and processes
- Geological and Geophysical Studies
- Geological Studies and Exploration
- Botany and Geology in Latin America and Caribbean
- Geological and Geophysical Studies Worldwide
- Latin American Legal and Economic Studies
- Geochemistry and Geologic Mapping
- Cardiac, Anesthesia and Surgical Outcomes
- Image Processing and 3D Reconstruction
- Abdominal Surgery and Complications
- Arctic and Russian Policy Studies
- Historical and socio-economic studies of Spain and related regions
- Seismic Waves and Analysis
- Karst Systems and Hydrogeology
- Cryospheric studies and observations
- Landslides and related hazards
- Groundwater and Watershed Analysis
- Geophysical and Geoelectrical Methods
- High-pressure geophysics and materials
National Polytechnic School
2018-2021
Instituto Geofísico de la Escuela Politécnica Nacional
2014-2017
Actively growing folds can either have a propagating tip or be amplified in breadth through fixed tip. Whatever the growth mechanism, drainage network adapts to newly created tectonic slopes. Lithological resistance erosion, as well climate and uplift rates, exerts control on bedrock incision rates and, therefore, whether transverse river maintains its course finally is deflected. In southeastern Ecuador, northernmost end of Cutucú Uplift corresponds Macuma anticline, north-plunging...
Abstract The Quito Basin, a narrow NE‐trending tectonic depression, contains perched Quaternary volcaniclastic sequence juxtaposed against the Interandean Depression through fault system (QFS). Syntectonic infilling, which occurs during piggy‐back phase, consists of alluvial fan sets grading eastward into lacustrine facies. western piedmont margin overlies foothills volcanoes. Classic thrust models predict basinward propagation low‐angle thrusts ahead master faults. A magnetotelluric survey...