The formation of large tin-tungsten (Sn-W) deposits around granitic intrusions requires the
circulation of large volumes of fluids within permeable structures. Half of the world's tungsten …

Slip accommodation in subduction zones ranges from aseismic slip phenomena to regular
megathrust earthquakes, and strongly depends on pore fluid pressure. We develop a new …

Massive greisens are commonly associated with Sn‐W mineralization and constitute low‐
grade high‐tonnage deposits. The formation of this type of deposit results from an intense …

In the first kilometers of the subsurface, temperature anomalies due to heat conduction
processes rarely exceed 20–30∘ C. When fault zones are sufficiently permeable, fluid flow …

Heat from inflowing magma may act to seal permeable networks that assist passive
outgassing at volcanic conduit margins and in overlying domes, reducing the efficiency of …

Hydrothermal circulation through oceanic crust, and all the transfers of mass and heat
caused by this circulation, are controlled by the evolving permeability of the altered basaltic …

Rock texture and structure play an important role in the formation of the rock physical
properties, and also carry information about their genesis. The paper deals with the …

Porosity and permeability are key controls on hydrothermal circulation and alteration in
magmatically heated upper oceanic crust. However, the hydraulic properties of basalts …

Fluid flow through crustal rocks is controlled by permeability. Underground fluid flow is
crucial in many geotechnical endeavors, such as CO2 sequestration, geothermal energy …

Аннотация Текстура и структура горных пород играют существенную роль в
формировании их физических свойств, а также несут информацию о генезисе. В …