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Frank Mattern, Andreas Scharf, Abdul Razak Al-Sayigh, Nada Al-Wahaibi, Laura Galluccio, Gianluca Frijia and Mazin Al-Salmani
The study improves the understanding of the basal part of the Eocene Seeb Formation of Oman, informally known as ?Unit 1?, in terms of microfacies, lithostratigraphy and shale migration within the context of regional tectonics. We logged four sections be...
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Dmitry A. Ruban
The Late Miocene evolution of the Eastern Paratethys Sea was marked by significant palaeogeographical transformations. The knowledge of them should be improved with the information from the peripheral parts of this semi-enclosed marine basin. The study a...
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Evangelos Spyrou, Maria V. Triantaphyllou, Theodora Tsourou, Emmanuel Vassilakis, Christos Asimakopoulos, Aliki Konsolaki, Dimitris Markakis, Dimitra Marketou-Galari and Athanasios Skentos
Geological heritage or geoheritage refers to the total of geosites, i.e., areas of high geological interest in a given area. Geosites have a high potential of attracting geotourists, thus contributing to the development of the local economy. Assessing si...
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Gregory P. De Pascale
Pág. 175 - 183
Understanding the location and nature of Quaternary active crustal faults is critical to reduce both the impact of fault rupture and strong ground motions hazards (when these faults rupture causing earthquakes). It is also important for understanding how...
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Azra Khosravichenar, Morteza Fattahi, Hamideh Amini and Hans von Suchodoletz
Fluvial sediments are valuable paleoenvironmental archives of the Quaternary. Since besides environmental factors they are also affected by local tectonics or intrinsic processes, large instead of small catchments should be studied. In drylands covering ...
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Antonio Banko, Tedi Bankovic, Marko Pavasovic and Almin Ðapo
Over the years, Global Navigation Satellite Systems (GNSS) have been established in the geosciences as a tool that determines the positions of discrete points (stations) on the Earth?s surface, on global to local spatial scales in a very simple and econo...
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Enrico Miccadei, Cristiano Carabella, Giorgio Paglia and Tommaso Piacentini
This work analyzes the role of paleo-drainage network, morphotectonics, and surface processes in landscape evolution in a sector of the transition zone between the chain and the piedmont area of Central Apennines. Particularly, it focuses on the Verde St...
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Gabriel Vargas Easton,Sofía Rebolledo,Sergio A. Sepúlveda,Alfredo Lahsen,Ricardo Thiele,Brian Townley,Cristóbal Padilla,Rodrigo Rauld,Maria José Herrera,Marisol Lara
Pág. 141 - 171
The Liquiñe-Ofqui fault zone (LOFZ) in the Patagonian Andes is an active major transpressional intra-arc fault system along which Quaternary faulting and volcanism develop. Subaerial and submarine geomorphologic and structural characterization of latest ...
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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...
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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...
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