Recent studies have demonstrated a linkage between the crustal architecture and the
location of magmatic–hydrothermal Cu deposits in collisional orogens. However, if and how …

Ultra-high temperature (UHT) metamorphism is a significant feature of the Greater
Himalayan Crystalline complex (GHC), which constrains the dynamics of continental …

Understanding the rheology of orogenic wedges requires the knowledge of the structural
and thermal evolution of collisional units. In this study, we document the maximum …

The rheology of crystalline units controls the large‐scale deformation geometry and
dynamics of collisional orogens. Defining a time‐constrained rheological evolution of such …

In continental collisional orogenic belts, the hinterland-foreland transition plays a crucial role
in the deformation styles and in the exhumation modes of the middle crustal rocks. The …

Structural, kinematic and geothermometry analyses are applied to unravel the structural
evolution of the Ailao Shan Tectonic belt (ALTB) with a specific goal of understanding how …

Large hot orogens (LHO) are characterized by an increase in heat the production and
thickness of the lithosphere. The increase in heat production, related to the accretion of …

Low-viscosity channel flow, originating from a melt-weakened mid-crustal layer, is one of the
most popular tectonic models to explain the exhumation of deep-seated rocks in the Greater …

This is a techno-economic study probing the feasibility of power generation through
Enhanced Geothermal System (EGS) in Pakistan. The concept surrounds around providing …

The collision of continental crust results in the formation of orogenic wedges to
accommodate convergence. We use 2D thermomechanical models to address the growth of …