|
|
|
|
|
Danilo Morelli, Michele Locatelli, Nicola Corradi, Paola Cianfarra, Laura Crispini, Laura Federico and Sébastien Migeon
The review of recent bathymetric and geophysical data collected in the framework of several research and cartographic projects have allowed a detailed reconstruction of the morpho-structural setting and the (neo)tectonic evolution for both the Alpine and...
ver más
|
|
|
|
|
|
|
|
|
|
|
Malcolm D. J. MacDougall, Alexander Braun and Georgia Fotopoulos
The evolution of the passive margin off the coast of Eastern Canada has been characterized by a series of rifting episodes which caused widespread extension of the lithosphere and associated structural anomalies, some with the potential to be classified ...
ver más
|
|
|
|
|
|
|
|
|
|
|
Enrico Miccadei, Cristiano Carabella and Giorgio Paglia
Drainage basin-scale morphometric analysis and morphological evidence of tectonics represent helpful tools to evaluate and investigate morphoneotectonic processes in tectonically active regions. In this perspective, we applied an integrated analysis to t...
ver más
|
|
|
|
|
|
|
|
|
|
|
Mauro De Donatis, Mauro Alberti, Mattia Cipicchia, Nelson Muñoz Guerrero, Giulio F. Pappafico and Sara Susini
Field work on the search and characterization of ground effects of a historical earthquake (i.e., the Cagli earthquake in 1781) was carried out using terrestrial and aerial digital tools. The method of capturing, organizing, storing, and elaborating digi...
ver más
|
|
|
|
|
|
|
|
|
|
|
Martina Misuraca, Francesca Budillon, Renato Tonielli, Gabriella Di Martino, Sara Innangi and Luciana Ferraro
A closely spaced set of high-resolution Chirp-Sonar and Sparker profiles and swath bathymetric data was acquired in 2013 for the I-AMICA Project off the Volturno River mouth (Southern Tyrrhenian Sea) by the Istituto per l?Ambiente Marino Costiero (IAMC),...
ver más
|
|
|
|
|
|
|
|
|
|
|
Giovanni Barreca, Marta Corradino, Carmelo Monaco and Fabrizio Pepe
The offshore margin of Mt. Etna has been shaped by Middle Pleistocene to Holocene shortening and extension and, more recently, by gravity-related sliding of the volcanic edifice. These processes have acted contemporaneously although the gravitational com...
ver más
|
|
|
|
|
|
|
|
|
|
|
Fenando Martínez,César Arriagada,Constantino Mpodozis,Matías Peña
Pág. 258 - 278
The Triassic and Jurassic tectonic history of northern Chile has been dominated by extension, althoughclear evidence about the nature and geometry of the extensional basins and subsequent inversion structures has beenadequately illustrated in only a few ...
ver más
|
|
|
|
|
|
|
|
|
|
|
Christian Creixell,Miguel angel Parada,Diego Morata,Paulina Vasquez,Carlos Perez de Arce,Cesar Arriagada
Pág. 37 - 63
The Middle-Late Jurassic mafic dike swarms of central Chile between 33º and 33º45'S register the tectonic activity of the contemporaneous arc represented by the Coastal batholith. These dike swarms evidence alternate episodes of transtension and transpre...
ver más
|
|
|
|
|
|
|
|
|
|
|
Juan Pablo Radic
Pág. 220 - 246
The Cordillera Principal at 36 to 39°S is an excellent place to address the relationship between tectonics and volcanism. Based on tectonostratigraphic analysis of the Cenozoic basins it has been possible to recognize a clear spatial coincidence between ...
ver más
|
|
|
|
|
|
|
|
|
|
|
Hans Niemeyer,Gabriel Gonzalez,Edmundo Martinez-De Los Rios
Pág. 165 - 186
RESUMEN. El margen continental en las inmediaciones de Antofagasta puede subdividirse en tres dominios morfoestructurales: Cordillera de la Costa, plataforma costera y talud continental. La Cordillera de la Costa se encuentra separada de la plataforma co...
ver más
|
|
|
|
|
|