For most nongeologists, the idea of liquids\ud moving through solid rock is a\ud strange one. But liquids of one sort or\ud another are thought to be ubiquitous in the\ud Earth. There are the familiar hydrothermal\ud fluids, dominated by water, which occur in\ud the very shallow crust (the Old Faithful\ud geyser in Yellowstone National Park in the\ud United States is a dramatic example). But in\ud the deeper parts of the Earth there are\ud hydrous and carbon dioxide (CO2) liquids\ud formed by the heating of rocks as the minerals\ud containing these molecules break down
Throughout Earth, rocks respond to changing physical and chemical conditions by converting one rock ...
International audienceThe link between volatiles and mantle melting has so far been illuminated by e...
This paper reviews the origin and evolution of fluid inclusions in ultramafic xenoliths, providing a...
For most nongeologists, the idea of liquids moving through solid rock is a strange one. But liquid...
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...
The stony part of the Earth is solid under normal conditions at the present day. Volcanism is the e...
International audienceVolatiles and melts are thoroughly related in the Earth's mantle because volat...
The liquid state dominates terrestrial and planetary processes. The history of the early solar syste...
The motion of aqueous and magmatic liquids has a large influence on the evolution of the cooling an...
Interaction of rocks with fluids can significantly change mineral assemblage and structure. This so-...
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...
For more than half a century, thought about granite genesis and crustal evolution has been guided by...
Throughout Earth, rocks respond to changing physical and chemical conditions by converting one rock ...
International audienceThe link between volatiles and mantle melting has so far been illuminated by e...
This paper reviews the origin and evolution of fluid inclusions in ultramafic xenoliths, providing a...
For most nongeologists, the idea of liquids moving through solid rock is a strange one. But liquid...
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...
The stony part of the Earth is solid under normal conditions at the present day. Volcanism is the e...
International audienceVolatiles and melts are thoroughly related in the Earth's mantle because volat...
The liquid state dominates terrestrial and planetary processes. The history of the early solar syste...
The motion of aqueous and magmatic liquids has a large influence on the evolution of the cooling an...
Interaction of rocks with fluids can significantly change mineral assemblage and structure. This so-...
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...
For more than half a century, thought about granite genesis and crustal evolution has been guided by...
Throughout Earth, rocks respond to changing physical and chemical conditions by converting one rock ...
International audienceThe link between volatiles and mantle melting has so far been illuminated by e...
This paper reviews the origin and evolution of fluid inclusions in ultramafic xenoliths, providing a...