Activity along the Osning Thrust in Central Europe during the Lateglacial: ice-sheet and lithosphere interactions
C Brandes, J Winsemann, J Roskosch… - Quaternary Science …, 2012 - Elsevier
The Osning Thrust is one of the major fault systems in Central Europe, with a length of
approximately 115 km. It underwent a polyphase tectonic evolution in the Mesozoic that …
approximately 115 km. It underwent a polyphase tectonic evolution in the Mesozoic that …
A new 3D geological model and interpretation of structural evolution of the world-class Rio Tinto VMS deposit, Iberian Pyrite Belt (Spain)
A Martin-Izard, D Arias, M Arias, P Gumiel… - Ore Geology …, 2015 - Elsevier
A new 3D geological model and interpretation of structural evolution of the Rio Tinto world-
class VMS deposit are presented in this work. The Rio Tinto volcanogenic massive sulfide …
class VMS deposit are presented in this work. The Rio Tinto volcanogenic massive sulfide …
Geodynamic evolution of the Tatra Mts. and the Pieniny Klippen Belt (Western Carpathians): problems and comments
E Jurewicz - Acta Geologica Polonica, 2005 - geojournals.pgi.gov.pl
The geodynamic evolution of the Pieniny Klippen Belt (PKB) and the Tatra Mts. assumes
that: The Oravic-Vahic Basin developed due to Jurassic rifting processes with thinned …
that: The Oravic-Vahic Basin developed due to Jurassic rifting processes with thinned …
The deep-water fold-and-thrust belt offshore NW Borneo: Gravity-driven versus basement-driven shortening
The deep-water region offshore NW Borneo is an active fold-and-thrust belt that hosts a
significant number of proven hydrocarbon accumulations. In the past, two mechanisms have …
significant number of proven hydrocarbon accumulations. In the past, two mechanisms have …
Evolution of upper crustal faulting assisted by magmatic volatile release during early-stage continental rift development in the East African Rift
During the development of continental rifts, strain accommodation shifts from border faults to
intra-rift faults. This transition represents a critical process in the evolution of rift basins in the …
intra-rift faults. This transition represents a critical process in the evolution of rift basins in the …
Characterisation and diachronous initiation of coarse clastic deposition in the Magallanes–Austral foreland basin, Patagonian Andes
Abstract Magallanes–Austral Basin (MAB) fill is preserved along a> 1000 km north–south
trending outcrop belt in the southern Patagonia region of Argentina and Chile. Although the …
trending outcrop belt in the southern Patagonia region of Argentina and Chile. Although the …
[HTML][HTML] Impacts of data sampling on the interpretation of normal fault propagation and segment linkage
Throw-distance (TD) and throw-depth (TZ) plots are widely used by researchers and industry
to examine the growth of normal faults. This study uses high-quality three-dimensional (3D) …
to examine the growth of normal faults. This study uses high-quality three-dimensional (3D) …
The relationship between inverted normal faults and pure thrusting during the tectonic inversion of the Domeyko Cordillera, northern Chile: Structural and seismic …
The orogenic growth of the Domeyko Cordillera was induced by a positive tectonic
inversion. In this work, we have validated this interpretation from new field data, which were …
inversion. In this work, we have validated this interpretation from new field data, which were …
Seismic structure of the north‐central Chilean convergent margin: Subduction erosion of a paleomagmatic arc
E Contreras‐Reyes, J Becerra, H Kopp… - Geophysical …, 2014 - Wiley Online Library
We study the erosive convergent margin of north‐central Chile (at~ 31° S) by using high‐
resolution bathymetric, wide‐angle refraction, and multichannel seismic reflection data to …
resolution bathymetric, wide‐angle refraction, and multichannel seismic reflection data to …
Connecting seismically active normal faults with Quaternary geological structures in a complex extensional environment: The Colfiorito 1997 case history (northern …
The northern Apennines of Italy are characterized by a complex Tertiary tectonic history,
where superposed compressional and extensional deformation occurred. In such regions …
where superposed compressional and extensional deformation occurred. In such regions …