Chemical composition, genesis and exploration implication of garnet from the Hongshan Cu-Mo skarn deposit, SW China
In this study, we present new mineral chemical data on the garnet from the Hongshan Cu-
Mo deposit, one of the largest skarn deposits in the Sanjiang Tethyan tectonic domain, in …
Mo deposit, one of the largest skarn deposits in the Sanjiang Tethyan tectonic domain, in …
[HTML][HTML] Garnet U-Pb geochronology and geochemistry reveal deposit types and fluid evolution: An example from the Dongguashan Cu-Au deposit, eastern China
K Chen, Y Shao, J Zhang, Y Zhang, H Tan, Y Zhang… - Ore Geology …, 2022 - Elsevier
Dongguashan is one of the largest Cu-Au deposits in eastern China, with ubiquitous garnet
in the stratiform and skarn orebodies. The stratiform ore-formation remains enigmatic. In this …
in the stratiform and skarn orebodies. The stratiform ore-formation remains enigmatic. In this …
[HTML][HTML] Rapid, paced metamorphism of blueschists (Syros, Greece) from laser-based zoned Lu-Hf garnet chronology and LA-ICPMS trace element map**
Unravelling the timing and rate of subduction-zone metamorphism and H 2 O release
requires linking time to the compositional changes of petrogenetic indicator minerals in …
requires linking time to the compositional changes of petrogenetic indicator minerals in …
Recycling reduced iron at the base of magmatic orogens
The Earth's continental crust is thought to originate from melting of the mantle, but it is too
felsic and depleted in Fe relative to a primary mantle melt. This depletion in Fe is also …
felsic and depleted in Fe relative to a primary mantle melt. This depletion in Fe is also …
Garnet: Common mineral, uncommonly useful
Garnet is a widespread mineral in crustal metamorphic rocks, a primary constituent of the
mantle, a detrital mineral in clastic sediments, and an occasional guest in igneous rocks …
mantle, a detrital mineral in clastic sediments, and an occasional guest in igneous rocks …
Subduction and continental collision in the Neoproterozoic: Sanukitoid-like magmatism and paired metamorphism in SE Brazil
Collisional orogens are a periodic manifestation of plate tectonics on Earth. They form by the
amalgamation of continental blocks, and they take place along both active and passive …
amalgamation of continental blocks, and they take place along both active and passive …
Oxidized iron in garnets from the mantle transition zone
The oxidation state of iron in Earth's mantle is well known to depths of approximately 200
km, but has not been characterized in samples from the lowermost upper mantle (200–410 …
km, but has not been characterized in samples from the lowermost upper mantle (200–410 …
Origin of Late Cenozoic Abaga–Dalinuoer basalts, eastern China: Implications for a mixed pyroxenite–peridotite source related with deep subduction of the Pacific …
M Zhang, Z Guo - Gondwana Research, 2016 - Elsevier
Abstract Continental intraplate basalts (15.42–0.16 Ma) from Abaga–Dalinuoer volcanic field
(ADVF) in central Inner Mongolia of eastern China, as a part of Cenozoic volcanic province …
(ADVF) in central Inner Mongolia of eastern China, as a part of Cenozoic volcanic province …
Effects of oxygen fugacity on hydroxyl incorporation in garnet at 1–3 GPa and 800–1000 C and implications for water storage in the mantle
Garnet, an important mineral component in Earth's interior, usually contains minor water as
structural OH, but experimental data on OH incorporation in the mineral as a function of …
structural OH, but experimental data on OH incorporation in the mineral as a function of …
[HTML][HTML] Petrology of alkali gabbro from the Messum Crater, Namibia (Paranà-Etendeka Province)–Melting of metasomatized carbonated lithospheric mantle sources
Foid gabbros (alkali gabbros) are late-stage intrusive rocks into the alkaline core of the
Cretaceous Messum complex, an anorogenic ring complex belonging to the Etendeka Large …
Cretaceous Messum complex, an anorogenic ring complex belonging to the Etendeka Large …