Satellite remote sensing imagery is especially useful for geological investigations in
Antarctica because of its remoteness and extreme environmental conditions that constrain …

This study addresses the interplay between strain/stress fields and paleo-fluid migration in
the Southern Andean Volcanic Zone (SVZ). The SVZ coexists with the margin-parallel …

Listvenites normally form during hydrothermal/metasomatic alteration of mafic and ultramafic
rocks and represent a key indicator for the occurrence of ore mineralizations in orogenic …

Abstract The Lower-Middle Triassic Aghdarband Basin, NE Iran, consists of a strongly
deformed arc-related marine succession deposited along the southern margin of Eurasia in …

We conduct 2-D numerical modeling of the lithospheric thermal structure of the North China
Craton (NCC) on basis of twenty-four crustal velocity structure profiles. About five hundred …

In continental margins, large-scale, strike-slip fault-systems resulted from oblique subduction
commonly exhibit a complex pattern of faulting where major faults define the inland …

Oblique convergence and subsequent transpression kinematics can be considered as the
general situation in most convergent and strike-slip tectonic boundaries. To better …

Exhumed faults in granitoids along the Lanterman Fault-Rennick Graben Fault system
(northern Victoria Land, Antarctica) show superposed ductile to brittle deformation and …

We have analyzed the brittle structures in a key area of the Alps–Apennines transition zone
(NW-Italy): here two orogens have interfered with each other since Oligocene times …

Tectonic stress is one of the most active deformation factors in the Earth's crust. Therefore,
determinations of its mode of action and form of conversion are critical for guiding research …