In the upper crust, where hydraulic gradients are typically< 1 MPa km− 1, advective heat
transport is often effective for permeabilities k≥ 10− 16 m² and advective mass (solute) …

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

Crustal Heat Flow: A Guide to Measurement and Modelling is a handbook for geologists and
geophysicists who manipulate thermal data, particularly for petroleum exploration. In theory …

Major intrusions of granitic rocks are found in several tectonic settings and, in all cases,
crustal melts may contribute to the volumes of granitic magma. High-grade metamorphism …

At depths greater than several kilometers in the crust, elevated temperature, elevated
confining pressure, and the presence of reactive pore fluids typically drive rapid destruction …

Abstract In the Catalina Schist subduction-zone metamorphic complex (California),
metasedimentary rocks show a decrease in N concentration and an increase in δ 15 N air …

Fluid pressure in the crust may be controlled by different mechanisms according to depth,
temperature, and the mineralogy of the host rocks. Where rocks are fluid‐saturated, fluid …

Large volumes of greenhouse gases such as CH4 and CO2 form by contact metamorphism
of organic-rich sediments in aureoles around sill intrusions in sedimentary basins …

Magnetotelluric and multichannel seismic reflection measurements indicate that the
Phanerozoic lower continental crust is commonly electrically conductive and reflective, in …

Primary and pseudosecondary fluid inclusions occur in oscillatory-and sector-zoned
omphacite in eclogitic veins from the Monviso ophiolitic complex in the Western Alps. The …