AbstractAt peak granulite-facies metamorphic conditions, lower continental crust is arguably fluxed by large amounts of two key low water activity fluids: (i) high-density CO2 and/or (ii) concentrated saline solutions. These fluids are either internally-derived, generated by mineral reactions or dehydration melting or, notably for CO2, externally-derived, issued from the underlying mantle. Postmetamorphic evolution results in complete disappearance of these fluids, except for minute remnants preserved in minerals as fluid inclusions. Two major processes are involved: (i) at peak conditions, granitoid magmas form, migrate upward, and crystallize as shallow intrusions in the upper crust (mineralized porphyry types or reduced intrusions); (ii)...
AbstractThis paper reviews the origin and evolution of fluid inclusions in ultramafic xenoliths, pro...
Orogenic gold deposits are comprised of complex quartz vein arrays that form as a result of fluid fl...
The 11th Symposium on Polar Science/Ordinary sessions: [OG] Polar Geosciences, Wed. 2 Dec
AbstractAt peak granulite-facies metamorphic conditions, lower continental crust is arguably fluxed ...
At peak granulite-facies metamorphic conditions, lower continental crust is arguably fluxed by large...
The formation of continents involves a combination of magmatic and metamorphic processes. These proc...
AbstractThe formation of continents involves a combination of magmatic and metamorphic processes. Th...
AbstractHigh-grade dehydration of amphibolite-facies rocks to granulite-facies is a process that can...
The various models for the nature and origin of fluids in granulite facies metamorphism were summari...
Fluid infiltration into retrograde granulites of the Southern Marginal Zone (Limpopo high grade terr...
AbstractFluid infiltration into retrograde granulites of the Southern Marginal Zone (Limpopo high gr...
Lower crustal granulites, which constitute the base of all continents, belong to two series: high-pr...
The fluid phase plays an important role in many crustal processes, such as metamorphism, metasomatis...
AbstractDuring granulite-facies metamorphism of metasedimentary rocks by the infiltration of carboni...
The Southern Marginal Zone of the Limpopo Complex documents strong evidence that CO2-rich (XCO2=0.7–...
AbstractThis paper reviews the origin and evolution of fluid inclusions in ultramafic xenoliths, pro...
Orogenic gold deposits are comprised of complex quartz vein arrays that form as a result of fluid fl...
The 11th Symposium on Polar Science/Ordinary sessions: [OG] Polar Geosciences, Wed. 2 Dec
AbstractAt peak granulite-facies metamorphic conditions, lower continental crust is arguably fluxed ...
At peak granulite-facies metamorphic conditions, lower continental crust is arguably fluxed by large...
The formation of continents involves a combination of magmatic and metamorphic processes. These proc...
AbstractThe formation of continents involves a combination of magmatic and metamorphic processes. Th...
AbstractHigh-grade dehydration of amphibolite-facies rocks to granulite-facies is a process that can...
The various models for the nature and origin of fluids in granulite facies metamorphism were summari...
Fluid infiltration into retrograde granulites of the Southern Marginal Zone (Limpopo high grade terr...
AbstractFluid infiltration into retrograde granulites of the Southern Marginal Zone (Limpopo high gr...
Lower crustal granulites, which constitute the base of all continents, belong to two series: high-pr...
The fluid phase plays an important role in many crustal processes, such as metamorphism, metasomatis...
AbstractDuring granulite-facies metamorphism of metasedimentary rocks by the infiltration of carboni...
The Southern Marginal Zone of the Limpopo Complex documents strong evidence that CO2-rich (XCO2=0.7–...
AbstractThis paper reviews the origin and evolution of fluid inclusions in ultramafic xenoliths, pro...
Orogenic gold deposits are comprised of complex quartz vein arrays that form as a result of fluid fl...
The 11th Symposium on Polar Science/Ordinary sessions: [OG] Polar Geosciences, Wed. 2 Dec