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 …

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 …

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 …

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 …

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 …

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 …

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) …

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 …

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 …

We use two-and three-dimensional seismic reflection data from the deep-water Niger Delta
fold and thrust belt to document evidence for two, discrete, postfaulting deformation …