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Diego Aedo,Daniel Melnick,Ed Garrett,Mario Pino
Pág. 125 - 152
At Chaihuín marsh, south of Valdivia (39°56? S/73°33? W), a sand bed was deposited during the 1960 earthquake. The aim of this study is to map the 1960 tsunami deposit in detail and to associate earlier sand layers with past tsunamis. Geologic field mapp...
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Daniel Melnick,Marcos Moreno,Marco Cisternas,Andrés Tassara
Pág. 558 - 563
The Maule earthquake (Mw 8.8) that affected south-central Chile on February 27, 2010 was preceded by the 1835 event documented by FitzRoy and Darwin. The relation between both events has remained controversial. Fault slip in 2010 estimated by Lorito et a...
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Gabriel Vargas,Marcelo Farias,Sebastien Carretier,Andres Tassara,Stephane Baize,Daniel Melnick
Pág. 219 - 238
On February 27, 2010 at 03:34:08 AM an Mw8.8 earthquake, with epicenter located off Cobquecura (73.24°W; 36.29°S), severely hit Central Chile. The tsunami waves that followed this event affected the coastal regions between the cities of Valparaíso and Va...
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Barnsley, R. Peacock, N. J. Dunn, J. Melnick, I. M. Coffey, I. H. Rainnie, J. A. Tarbutt, M. R. Nelms, N.
Pág. 2388 - 2408
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Andres Folguera,Victor Ramos,Daniel Melnick
Pág. 227 - 240
The Neuquén Andes between 36 and 39°S were built by a broad range of processes during the last 30 Ma. Periods of deformation can be classified in two alternating types: periods of extension associated with homogeneous shear parallel to the trench, whose ...
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Shmulevich, I; Melnick, V; Egiazarian, K
Pág. 189 - 192
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