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Luisa Fernanda Echeverría-King, Jorge Pinto, María Angela Lorena Mosquera-Montoya
Pág. e1672
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Ana Luísa Guimarães Ribeiro,Willian Barros Sidião,Pedro Henrique Pinto Ribeiro,Ademilson Coneglian,Dywre Bento da Costa
Objetivou-se com o presente estudo, equacionar a tendência do balanço hídrico, temperatura e umidade relativa nos anos de 2009 a 2014, na região de Uberlândia-MG, comparando-os com aqueles da série histórica do período de 1981 a 2014. Foi utilizado o mét...
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Manolo Trindade Quintilhan,Weslley Candido de Oliveira,Aylson Costa Oliveira,Bárbara Luísa Corradi Pereira,Romulo Môra,Adrianna Amorim de Sousa Pinto
A durabilidade natural da madeira é essencial na definição do seu uso. Assim, objetivou-se avaliar a deterioração ao longo de 12 meses da madeira tratada e não tratada de Corymbia citriodora, Eucalyptus camaldulensis x Eucalyptus grandis, e Euc...
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Sebastian Herrera, Luisa Pinto, Katja Deckart, Javier Cortés, Javier Valenzuela
Pág. 87 - 122
Crustal thickening by horizontal shortening and associated deformation have been broadly considered as
prime mechanisms for mountain building in the Central Andes of western South America. However, timing and structural
style of Andean orogeny in norther...
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Carolina Muñoz-Sáez,Luisa del Carmen Pinto,Reynaldo Charrier,Thierry Nalpas
Pág. 1 - 28
The current paper analyzes the evolution of the Abanico Basin, exposed in the Chilean Principal Cordillera in central Chile (33º-35ºS). According to previous studies, the basin has been affected by two main deformational episodes; the first, related to e...
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Katja Deckart,Katherine Pinochet,Sergio A. Sepúlveda,Luisa C. Pinto,Stella M. Moreiras
Pág. 248 - 258
The Mesón Alto chaotic deposit, located in the Main Cordillera at about 33°40?S, is an important landform with a volume of ca. 4.5 km3 unconsolidated material deposited downstream of the Yeso Dam in the Yeso Valley, Río Maipo drainage basin. Historical w...
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Daniel González,Luisa Pinto,Matías Peña,César Arriagada
Pág. 295 - 316
Regional and local strike-slip systems in Chile are complex and pose interesting questions, such as theinteraction between strike-slip and reverse faults, how they evolve, and the relationship between shortening, rotationand uplift. Within this context, ...
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Luisa Pinto,Gerard Herail,Reynaldo Charrier
Pág. 19 - 44
In northern Chile (18-20°S), the western border of the high Andean Plateau (Altiplano) was uplifted by high-angle thrust faults and associated folds. These developed along the Precordillera, which is the morphostructural unit that connects the Andean Pla...
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