A series of hydrothermal piston-cylinder experiments have been performed to determine the composition of representative fluids and fluid/melt/rock interaction in subduction zones. Experiments were conducted under H2O saturated conditions at 2.2 GPa over a temperature range from 600–750 °C. The experiments contained synthetic, trace-element-doped pelitic starting material and fractured quartz chips to trap and preserve synthetic fluid/melt inclusions. Pelite residues from the subsolidus experiments (600–650 °C) consist of an eclogite-facies mineral assemblage including quartz, phengite, epidote, rutile, garnet, amphibole, apatite, and zircon. Coexisting hydrous fluids are expected to be completely buffered for trace elements by this mineral ...
The phase and melting relations in subducted pelites have been investigated experimentally at condit...
Serpentinites release at sub-arc depths volatiles and several fluid-mobile trace elements found in a...
Aqueous vapour, released from subducted dehydrated oceanic crust, has the potential to remove relati...
A series of hydrothermal piston-cylinder experiments have been performed to determine the compositio...
A series of hydrothermal piston-cylinder experiments have been performed to determine the compositio...
The fluid inclusions preserved in high and ultrahigh pressure rocks provide direct information on th...
High-pressure (HP) and ultra-high pressure (UHP) terranes are excellent natural laboratories to stud...
High-pressure (HP) and ultra-high pressure (UHP) terranes are excellent natural laboratories to stud...
The phase and melting relations in subducted pelites have been investigated experimentally at condit...
High-pressure (HP) and ultra-high pressure (UHP) terranes are excellent natural laboratories to stud...
The partitioning of major and trace elements between eclogite and aqueous fluids with variable salin...
Both silicate melts and aqueous fluids are thought to play critical roles in the chemical differenti...
Permeabilities in the subducting stab appear to be too low and dihedral angles between fluid and rel...
We review three case studies emphasizing the role of ultramafic rocks in the recycling of volatiles ...
We report the results of experiments on two natural marine sediments with different carbonate conten...
The phase and melting relations in subducted pelites have been investigated experimentally at condit...
Serpentinites release at sub-arc depths volatiles and several fluid-mobile trace elements found in a...
Aqueous vapour, released from subducted dehydrated oceanic crust, has the potential to remove relati...
A series of hydrothermal piston-cylinder experiments have been performed to determine the compositio...
A series of hydrothermal piston-cylinder experiments have been performed to determine the compositio...
The fluid inclusions preserved in high and ultrahigh pressure rocks provide direct information on th...
High-pressure (HP) and ultra-high pressure (UHP) terranes are excellent natural laboratories to stud...
High-pressure (HP) and ultra-high pressure (UHP) terranes are excellent natural laboratories to stud...
The phase and melting relations in subducted pelites have been investigated experimentally at condit...
High-pressure (HP) and ultra-high pressure (UHP) terranes are excellent natural laboratories to stud...
The partitioning of major and trace elements between eclogite and aqueous fluids with variable salin...
Both silicate melts and aqueous fluids are thought to play critical roles in the chemical differenti...
Permeabilities in the subducting stab appear to be too low and dihedral angles between fluid and rel...
We review three case studies emphasizing the role of ultramafic rocks in the recycling of volatiles ...
We report the results of experiments on two natural marine sediments with different carbonate conten...
The phase and melting relations in subducted pelites have been investigated experimentally at condit...
Serpentinites release at sub-arc depths volatiles and several fluid-mobile trace elements found in a...
Aqueous vapour, released from subducted dehydrated oceanic crust, has the potential to remove relati...