Veins are common features in rocks and extremely useful structures to determine stress,
strain, pressure, temperature, fluid composition and fluid origin during their formation. Here …

Core-complex formation driven by lithospheric extension is a first-order process of heat and
mass transfer in the Earth. Core-complex structures have been recognized in the continents …

Compressional intracontinental orogens are major zones of crustal thickening produced at
large distances from active plate boundaries. Consequently, any account of their initiation …

A review of coupled groundwater and heat transfer theory is followed by an introduction to
geothermal measurement techniques. Thereafter, temperaturedepth profiles (geotherms) …

The Neogene elevation history of the Mount Everest region is key for understanding the
tectonic history of the world's highest mountain range, the evolution of the Tibetan Plateau …

Unconformity-related hydrothermal ore deposits typically form by mixing of hot, deep, rock-
buffered basement brines and cooler fluids derived from the surface or overlying sediments …

Hydrofractures, or hydraulic fractures, are fractures where a significantly elevated fluid
pressure played a role in their formation. Natural hydrofractures are abundant in rocks and …

Hydrothermal deposits in extensional settings are common worldwide. These deposits are
generally assumed to have formed from circulating fluids that mix with other fluids. However …

This study investigates the Late Aptian–earliest Albian platform carbonates of the
Benicàssim area (Maestrat Basin, Spain) in order to assess the relationship between bed …

The hydrodynamic consequences of a glaciation/deglaciation cycle within an intercratonic
sedimentary basin on subsurface transport processes is assessed using numerical models …