For most nongeologists, the idea of liquids moving through solid rock is a strange one. But liquids of one sort or another are thought to be ubiquitous in the Earth. There are the familiar hydrothermal fluids, dominated by water, which occur in the very shallow crust (the Old Faithful geyser in Yellowstone National Park in the United States is a dramatic example). But in the deeper parts of the Earth there are hydrous and carbon dioxide (CO2) liquids formed by the heating of rocks as the minerals containing these molecules break down
This paper reviews the origin and evolution of fluid inclusions in ultramafic xenoliths, providing a...
In the late 18th century, Neptunists and Plutonists had controversial opinions about the formation o...
Metamorphic hydrous, CO2-bearing fluids play a critical role in the global carbon cycle. However, ho...
For most nongeologists, the idea of liquids\ud moving through solid rock is a\ud strange one. But li...
Most of the phenomena studied by geologists and geochemists are due, at least in part, to the abil...
Most of the Earth's mass is solid. The crust and mantle of the Earth extend down almost 3000 km and...
Investigation of the effect of volatile materials on the melting temperatures of rocks suggests that...
International audienceVolatiles and melts are thoroughly related in the Earth's mantle because volat...
The stony part of the Earth is solid under normal conditions at the present day. Volcanism is the e...
The motion of aqueous and magmatic liquids has a large influence on the evolution of the cooling an...
The liquid state dominates terrestrial and planetary processes. The history of the early solar syste...
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...
International audienceThe link between volatiles and mantle melting has so far been illuminated by e...
For more than half a century, thought about granite genesis and crustal evolution has been guided by...
This paper reviews the origin and evolution of fluid inclusions in ultramafic xenoliths, providing a...
In the late 18th century, Neptunists and Plutonists had controversial opinions about the formation o...
Metamorphic hydrous, CO2-bearing fluids play a critical role in the global carbon cycle. However, ho...
For most nongeologists, the idea of liquids\ud moving through solid rock is a\ud strange one. But li...
Most of the phenomena studied by geologists and geochemists are due, at least in part, to the abil...
Most of the Earth's mass is solid. The crust and mantle of the Earth extend down almost 3000 km and...
Investigation of the effect of volatile materials on the melting temperatures of rocks suggests that...
International audienceVolatiles and melts are thoroughly related in the Earth's mantle because volat...
The stony part of the Earth is solid under normal conditions at the present day. Volcanism is the e...
The motion of aqueous and magmatic liquids has a large influence on the evolution of the cooling an...
The liquid state dominates terrestrial and planetary processes. The history of the early solar syste...
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...
International audienceThe link between volatiles and mantle melting has so far been illuminated by e...
For more than half a century, thought about granite genesis and crustal evolution has been guided by...
This paper reviews the origin and evolution of fluid inclusions in ultramafic xenoliths, providing a...
In the late 18th century, Neptunists and Plutonists had controversial opinions about the formation o...
Metamorphic hydrous, CO2-bearing fluids play a critical role in the global carbon cycle. However, ho...