This is the first detailed report and analyses of deformation from the W part of the Deccan
large igneous province (DLIP), Maharashtra, India. This deformation, related to the India …

Based on a review of published literature and on the report of a few case studies, this paper
summarizes the state of the art on paleostress determinations by fault slip data inversions …

Two orogenic belts have been recognized in south-east Brazil, which are interpreted to have
been formed as a product of diachronous collisions between three continental plates. Wide …

The Monte Alpi (southern Italy) is well known as an outcropping analogue of the Val d'Agri
subsurface units which host a number of oil fields of economic importance. This paper …

Fingerprints of the opening of the Western Black Sea Basin and collision of Pontides and
Sakarya Continent along the Intra-Pontide suture can be traced in the area between Cide …

Shear zone patterns within the Suretta nappe of the Swiss Alps are studied in order to
understand finite strain and bulk tectonic displacements. The Suretta nappe is chosen for …

The Novate intrusion is a Late Alpine leucogranite that intruded the structures related to
dextral back‐thrusting along the Periadriatic Fault System in the Eastern Central Alps. The …

This paper aims at reconstructing paleostress history and deciphering the pore-fluid
pressure conditions during the reactivation of a regional-scale fault. Paleostress analyses of …

Abstract The Gran Paradiso nappe of the northwestern Alps mostly consists of augen
gneisses derived from the Alpine deformation of Permian granitoids. The regional foliation of …

The extent to which persistent, rather than transient, fissures (wide planar voids) can exist
along upper crustal faults is important in assessing fault permeability to mineral and …