Phanerozoic tin and tungsten mineralization—Tectonic controls on the distribution of enriched protoliths and heat sources for crustal melting
Phanerozoic primary tin and tungsten deposits and lithium–cesium–tantalum (LCT) type
pegmatites define discontinuous belts that reach several thousand kilometers length …
pegmatites define discontinuous belts that reach several thousand kilometers length …
Collision vs. subduction-related magmatism: two contrasting ways of granite formation and implications for crustal growth
Earth's continental crust is dominantly made of buoyant, felsic igneous material (granitoids),
that was ultimately extracted from the mantle as a result of Earth's differentiation. Since felsic …
that was ultimately extracted from the mantle as a result of Earth's differentiation. Since felsic …
The role of continental subduction in mantle metasomatism and carbon recycling revealed by melt inclusions in UHP eclogites
Subduction is the main process that recycles surface material into the mantle. Fluids and
melts derived by dehydration and partial melting reactions of subducted continental crust, a …
melts derived by dehydration and partial melting reactions of subducted continental crust, a …
Post-collisional magmatism: Crustal growth not identified by zircon Hf–O isotopes
The combination of U–Pb, Lu–Hf and O isotopic analyses in global zircon databases has
recently been used to constrain continental crustal growth and evolution. To identify crust …
recently been used to constrain continental crustal growth and evolution. To identify crust …
Protracted, coeval crust and mantle melting during Variscan late-orogenic evolution: U–Pb dating in the eastern French Massif Central
The late stages of the Variscan orogeny are characterized by middle to lower crustal melting
and intrusion of voluminous granitoids throughout the belt, which makes it akin to “hot” …
and intrusion of voluminous granitoids throughout the belt, which makes it akin to “hot” …
Flow of partially molten crust controlling construction, growth and collapse of the Variscan orogenic belt: the geologic record of the French Massif Central
O Vanderhaeghe, O Laurent… - Bulletin de la …, 2020 - pubs.geoscienceworld.org
Flow of partially molten crust controlling construction, growth and collapse of the Variscan
orogenic belt: the geologic record of the French Massif CentralImpact du fluage de la croûte …
orogenic belt: the geologic record of the French Massif CentralImpact du fluage de la croûte …
New insights into the crustal growth of the Paleoproterozoic margin of the Archean Kéména-Man domain, West African craton (Guinea): Implications for gold mineral …
Abstract The Baoulé-Mossi Paleoproterozoic domain on the West African Craton is known
for its world-class orogenic gold deposits formed during the Eburnean orogeny between ca …
for its world-class orogenic gold deposits formed during the Eburnean orogeny between ca …
Appinite suites and their genetic relationship with coeval voluminous granitoid batholiths
JB Murphy - International Geology Review, 2020 - Taylor & Francis
Appinite complexes preserve evidence of mantle processes that produce voluminous
granitoid batholiths. These plutonic complexes range from ultramafic to felsic in composition …
granitoid batholiths. These plutonic complexes range from ultramafic to felsic in composition …
40 Ma of hydrothermal W mineralization during the Variscan orogenic evolution of the French Massif Central revealed by U-Pb dating of wolframite
We present U-Pb thermal ionization mass spectrometer (TIMS) ages of wolframite from
several granite-related hydrothermal W±Sn deposits in the French Massif Central (FMC) …
several granite-related hydrothermal W±Sn deposits in the French Massif Central (FMC) …