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Juan Luis Alonso
Juan Luis Alonso
Universidad de Oviedo (Professor, retired)
Verified email at uniovi.es
Title
Cited by
Cited by
Year
A thin skinned tectonics model for an arcuate fold and thrust belt: the Cantabrian Zone
A Pérez-Estaún, F Bastida, JL Alonso, JL Marquínez, J Aller, ...
Tectonics 7, 517-537, 1988
3871988
W5 Tertiary basins and Alpine tectonics in the Cantabrian Mountains (NW Spain)
JL Alonso, J Pulgar, J García-Ramos, P Barba
Tertiary basins of Spain: the stratigraphic record of crustal kinematics, 1996
3701996
Seismic image of the Cantabrian Mountains in the western extension of the Pyrenees from integrated ESCIN reflection and refraction data
JA Pulgar, J Gallart, G Fernández-Viejo, J Alvarez-Marrón, EGJL Alonso, ...
Tectonophysics 264, 1-20, 1996
1841996
Paleogeographic inversion resulting from large out of sequence breaching thrusts: The León Fault (Cantabrian Zone, NW Iberia). A new picture of the external Variscan Thrust …
JL Alonso, A Marcos, A Suárez
Geologica Acta 7 (4), 0451-473, 2009
1832009
Origin and significance of olistostromes in the evolution of orogenic belts: A global synthesis
A Festa, K Ogata, GA Pini, Y Dilek, JL Alonso
Gondwana Research 39, 180-203, 2016
1762016
La deformación alpina en el basamento varisco de la Zona Cantábrica
JA Pulgar, JL Alonso, RG Espina, JA Marín
Trabajos de geologia, 283-295, 1999
1471999
Crustal structure of the external variscides in northwest Spain from deep seismic reflection profiling
A Pérez-Estaún, JA Pulgar, E Banda, JENRG Alvarez-Marrón
Tectonophysics 232, 91-118, 1994
1201994
Sequences of thrusts and displacement transfer in the superposed duplexes of the Esla Nappe Region (Cantabrian Zone, NW Spain)
JL Alonso
Journal of Structural Geology 9 (8), 969-983, 1987
721987
Displacement transfer from borders to interior of a plate: A crustal transect of Iberia
L Quintana, JA Pulgar, JL Alonso
Tectonophysics 663, 378-398, 2015
672015
Estructura y evolución tectonoestratigráfica del Manto del Esla (Zona Cantábrica, NW de España)
JL Alonso
Publicaciones de la Diputación Provincial de León. Institución Fray …, 1987
62*1987
Extensional tectonics and gravitational collapse in an Ordovician passive margin: The Western Argentine Precordillera
JL Alonso, J Gallastegui, J García-Sansegundo, P Farias, LRR Fernández, ...
Gondwana Research 13 (2), 204-215, 2008
612008
Structure and organization of the Porma mélange: progressive denudation of a submarine nappe toe by gravitational collapse
JL Alonso, A Marcos, A Suárez
American Journal of Science 306 (1), 32-65, 2006
612006
Hinterland-foreland zonation of the Variscan orogen in the Central Pyrenees: comparison with the northern part of the Iberian Variscan Massif
J García-Sansegundo, J Poblet, JL Alonso, P Clariana
Geological Society, London, Special Publications 349 (1), 169-184, 2011
592011
Fold reactivation involving angular unconformable sequences. Theoretical analysis and natural examples from the Cantabrian Zone (NW Spain)
JL Alonso
Tectonophysics 170, 55-77, 1989
591989
El relieve de la Cordillera Cantábrica
JL Alonso, FJÁ Pulgar, D Pedreira
Enseñanza de las Ciencias de la Tierra 15 (2), 151-163, 2007
552007
Growth and propagation of buckle folds determined from syntectonic sediments (the Ubierna Fold Belt, Cantabrian Mountains, N Spain)
RG Espina, JL Alonso, JA Pulgar
Journal of Structural Geology 18 (4), 431-441, 1996
531996
Forelimb deformation in some natural examples of fault-propagation folds
JL Alonso, A Teixell
Thrust tectonics, 175-180, 1992
531992
The Pre-Andean Phases of Construction of the Southern Andes Basement in Neoproterozoic–Paleozoic Times
The Evolution of the Chilean-Argentinean Andes, 111-131, 2018
482018
Stratigraphy and structure of the southeastern Garona Dome
J Garcia-Sansegundo, J Luis Alonso
Geodinamica Acta 3 (2), 127-134, 1989
481989
Mélanges and other types of block-in-matrix formations in the Cantabrian Zone (Variscan Orogen, northwest Spain): origin and significance
JL Alonso, A Marcos, E Villa, A Súarez, OA Merino-Tomé, LP Fernández
International Geology Review, 563-580, 2015
462015
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