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Luis A. Lara-Valencia, Daniel Caicedo and Yamile Valencia-Gonzalez
Adaptation of Whale Optimization Algorithm (WOA) for optimum design of TMDs. Seismic performance is assessed using real accelerograms and an irregular case study. Effective, fast, and reliable methodology comparing to others in the literature. Practical ...
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Felipe Hermosilla Torres, José Luis Lara Arroyo
Pág. 101 - 117
En este trabajo se busca identificar algunos de los principales desafíos actuales de la profesión jurídica por medio del examen de la aplicación del liderazgo adaptativo a diversos escenarios propios del denominado derecho regulatorio, examinando la situ...
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Dr. Luis Silva Lara
Pág. 76
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Luis Silva Lara
Pág. 76
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Juan Jose Reyes,Silvana Vero,Ernesto Diaz-Rivera,Liliana Lara-Capistran LARA,Juan Noa,Luis Hernandez
Pág. 266 - 275
Postharvest diseases in fruits cause serious losses of fresh produce worldwide.The application of synthetic fungicides for the control of postharvest diseases such as anthracnose in mangoes can cause adverse effects on the environment and on human a...
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Mariana Peixoto Gomes, Lara Santos, José Luís Pinho and José S. Antunes do Carmo
Coastal zones currently face severe weaknesses and are subject to high-risk situations. Tropical storm events can contribute to the occurrence of these high-risk situations by causing storm surges with high water levels and, consequently, episodes of wav...
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Lara Dutra Silva, Eduardo Brito de Azevedo, Rui Bento Elias and Luís Silva
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Jon J. Major,Luis E. Lara
Pág. 196 - 215
Chaitén Volcano erupted unexpectedly in May 2008 in one of the largest eruptions globally since the 1990s. It was the largest rhyolite eruption since the great eruption of Katmai Volcano in 1912, and the first rhyolite eruption to have at least some of i...
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Álvaro Amigo,Luis E. Lara,Victoria C. Smith
Pág. 227 - 248
Tephra fall deposits and one large ignimbrite close to Chaitén and Michinmahuida Volcanoes were analyzed for chemistry and radiocarbon dated to correlate the eruptive units and establish the timing of eruptions. These data suggest that both volcanoes wer...
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Luis E. Lara,Rodrigo Moreno,Álvaro Amigo,Richard P. Hoblitt,Thomas C. Pierson
Pág. 249 - 261
Prior to May 2008, it was thought that the last eruption of Chaitén Volcano occurred more than 5,000 years ago, a rather long quiescent period for a volcano in such an active arc segment. However, increasingly more Holocene eruptions are being identified...
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Mirella Piña-Gauthier,Luis E. Lara,Klaus Bataille,Andrés Tassara,Juan C. Báez
Pág. 310 - 323
GPS data from stations around the Chaitén Volcano show a co-eruptive pattern of inflation and deflation that correlates well with the estimated effusion rate during the 2008-2009 eruption. Axisymmetric radial deflation is coeval with periods of fast dome...
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Eladio Arroyo Lara, Luis V. Pérez Gil
Los procesos en los que se han consolidado estructuras más o menos institucionalizadas de seguridad, permiten comprender el alcance y las limitaciones de la teoría de la integración en una etapa de hegemonía imperfecta, regida por dinámicas diferentes a ...
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Luis E. Lara
Pág. 125 - 130
On May 2, 2008 a Plinian eruption began on Chaiten volcano. Dome growing stage would have started on May 10-12 and extensive lahars and floods affected Chaiten town (ca. 5,000 inhabitants) on May 12. A volume up to ca. 4 km3 (non DRE) of rhyolitic magma ...
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Luis E. Lara,Jose A. Naranjo,Hugo Moreno
Pág. 241 - 258
Lanín volcano is a compound stratocone, mainly effusive, made up by four units defined through morphological criteria. The first unit represents an ancient volcano; the youngest three units form the present stratocone built since the Middle-Late Pleistoc...
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Jose A. Naranjo,Luis E. Lara
Pág. 359 - 366
During the winter months of August-September 2003 a small (VEI=0-1) eruption took place at the 9 km long fissure-like Nevados de Chillán Volcanic Complex (36°50'S), that includes Nuevo (formed between 1906 and 1945) and Arrau (formed in the 1973-1986 per...
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Renate M. Wall,Luis E. Lara
Pág. 243 - 258
The presence of Lower Miocene volcanic rocks in the Coastal Range of central Chile is unique in that the westernmost outcrops of the Oligocene-Miocene volcanic arc occur 80 km to the east. The Las Pataguas Lavas (LLP; 33,8°S) consists of a total exposed ...
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Luis Lara,Carolina Rodriguez,Hugo Moreno,Carlos Perez de Arce
Pág. 67 - 90
In the Andean Range, south of 39°S, there is a suite of eroded volcanic centres that includes remains of vents or proximal, intermediate or distal volcanic facies. New geochronological K-Ar data show that their ages are in the Late Pliocene-Middle Pleist...
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María Bermúdez,Ángel Rico,Álvaro Rodríguez,Luís Pena,Juan R. Rabuñal,Jerónimo Puertas,Luis Balairón,Ángel Lara,Enrique Aramburu,Felipe Morcillo,Miriam Castillo
Pág. 179 - 191
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María Bermúdez,Ángel Rico,Álvaro Rodríguez,Luís Pena,Juan R. Rabuñal,Jerónimo Puertas,Luis Balairón,Ángel Lara,Enrique Aramburu,Felipe Morcillo,Miriam Castillo
Pág. 179 - 191
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José Luis Gómez-Royuela, Almudena Majano-Majano, Antonio José Lara-Bocanegra, José Xavier and Marcelo F. S. F. de Moura
In the present work, single- and double-dowel joints following different geometric configurations are experimentally and numerically investigated to derive the splitting behaviour of beech wood (Fagus sylvatica L.), one of the most widespread hardwood sp...
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