Multistage anatexis during tectonic evolution from oceanic subduction to continental collision: A review of the North Qaidam UHP Belt, NW China
Abstract The North Qaidam ultra-high pressure (UHP) metamorphic belt in the northern
Tibetan Plateau is considered as a typical Alpine-type UHP metamorphic belt due to the …
Tibetan Plateau is considered as a typical Alpine-type UHP metamorphic belt due to the …
Conditions during the formation of granitic magmas by crustal melting–hot or cold; drenched, damp or dry?
Granitic magmas extracted from crustal sources can form over a wide variety of P, T and aH
2 O conditions. Both fluid-present and effectively fluid-absent conditions can yield granitic …
2 O conditions. Both fluid-present and effectively fluid-absent conditions can yield granitic …
Crustal melting vs. fractionation of basaltic magmas: Part 1, granites and paradigms
Granitoids are a major component of the continental crust. They play a pivotal role in its
evolution, either by adding new material (continental growth), or by reworking older …
evolution, either by adding new material (continental growth), or by reworking older …
Partial melting in the Higher Himalayan Crystallines of Eastern Nepal: the effect of decompression and implications for the 'Channel Flow'model
Partial melting of deep continental crust may occur during either prograde heating or
decompression. Although the effect of temperature on crustal melting has been widely …
decompression. Although the effect of temperature on crustal melting has been widely …
Intracontinental Eocene-Oligocene porphyry Cu mineral systems of Yunnan, western Yangtze Craton, China: compositional characteristics, sources, and implications …
Abstract The Yao'an porphyry Au system, Machangqing porphyry Cu-Mo system, and Beiya
porphyry-skarn Au system, are spatially and temporally associated with potassic felsic …
porphyry-skarn Au system, are spatially and temporally associated with potassic felsic …
Melted rocks under the microscope: microstructures and their interpretation
Recognising the former presence of melt in rocks which have undergone cooling and
exhumation over millions of years following regional metamorphism commonly relies on the …
exhumation over millions of years following regional metamorphism commonly relies on the …
The chemical behavior of fluids released during deep subduction based on fluid inclusions
This review combines fluid inclusion data from (HP-) UHP rocks with experimental research
and thermodynamic models to investigate the chemical and physical properties of fluids …
and thermodynamic models to investigate the chemical and physical properties of fluids …
Timescales of subduction initiation and evolution of subduction thermal regimes
Subduction zones are first-order features of plate tectonics on Earth, yet the mechanisms by
which subduction initiates remain enigmatic and controversial. Here, we reappraise the …
which subduction initiates remain enigmatic and controversial. Here, we reappraise the …
[HTML][HTML] What can we learn from melt inclusions in migmatites and granulites?
With less than two decades of activity, research on melt inclusions (MI) in crystals from rocks
that have undergone crustal anatexis–migmatites and granulites–is a recent addition to …
that have undergone crustal anatexis–migmatites and granulites–is a recent addition to …
Mechanisms of crustal anatexis: a geochemical study of partially melted metapelitic enclaves and host dacite, SE Spain
To shed light on the mechanisms of crustal anatexis, a detailed geochemical study has been
conducted on minerals and glasses of quenched anatectic metapelitic enclaves and their …
conducted on minerals and glasses of quenched anatectic metapelitic enclaves and their …