[HTML][HTML] Spatial and temporal control of Archean tectonomagmatic regimes
Secular trends in plutonic whole-rock geochemistry pose critical, although non-unique,
constraints to early Earth tectonics. Here, we present a large whole-rock geochemical (879 …
constraints to early Earth tectonics. Here, we present a large whole-rock geochemical (879 …
Current applications using key mineral phases in igneous and metamorphic geology: perspectives for the future
The study of magmatic and metamorphic processes is challenged by geological
complexities like geochemical variations, geochronological uncertainties and the …
complexities like geochemical variations, geochronological uncertainties and the …
High-pressure, halogen-bearing melt preserved in ultrahigh-temperature felsic granulites of the Central Maine Terrane, Connecticut (USA)
Inclusions of relic high-pressure melts provide crucial information on the fate of crustal rocks
in the deep roots of orogens during collision and crustal thickening, including at extreme …
in the deep roots of orogens during collision and crustal thickening, including at extreme …
The Laramide orogeny: Current understanding of the structural style, timing, and spatial distribution of the classic foreland thick-skinned tectonic system
The Laramide foreland belt comprises a broad region of thick-skinned, contractional
deformation characterized by an anastomosing network of basement-cored arches and …
deformation characterized by an anastomosing network of basement-cored arches and …
Into the high to ultrahigh temperature melting of earth's crust: investigation of melt and fluid inclusions within Mg-rich metapelitic granulites from the Mather Peninsula …
Precise constraints on the compositions of melts generated by anatexis under ultrahigh
temperature (UHT) conditions are critical for understanding processes of partial melting and …
temperature (UHT) conditions are critical for understanding processes of partial melting and …
The carbon budget of crustal reworking during continental collision: Clues from nanorocks and fluid inclusions
The source of volatiles in the continental crust is a long-standing issue. In addition to
controlling the amount of melt generated during anatexis, H 2 O and CO 2 budgets of the …
controlling the amount of melt generated during anatexis, H 2 O and CO 2 budgets of the …
Re-equilibration of quartz inclusions in garnet
Inclusion–host elastic thermobarometers are widely used to determine the pressure and
temperature (P–T) histories of metamorphic rocks. Complex metamorphic P–T paths can …
temperature (P–T) histories of metamorphic rocks. Complex metamorphic P–T paths can …
Halogen-bearing metasomatizing melt preserved in high-pressure (HP) eclogites of Pfaffenberg, Bohemian Massif
Primary granitic melt inclusions are trapped in garnets of eclogites in the garnet peridotite
body of Pfaffenberg, Granulitgebirge (Bohemian Massif, Germany). These polycrystalline …
body of Pfaffenberg, Granulitgebirge (Bohemian Massif, Germany). These polycrystalline …
Role and origin of water-fluxed melting in the generation of High Himalayan leucogranites
K Lei, XC Wang, SA Wilde - Journal of Asian Earth Sciences, 2024 - Elsevier
Abstract Knowledge of the role water has played in the evolution of Earth's continents is
crucial for improving our understanding of how its layers (eg crust and mantle) interact with …
crucial for improving our understanding of how its layers (eg crust and mantle) interact with …
First evidence of dmisteinbergite (CaAl2Si2O8 polymorph) in high-grade metamorphic rocks
We identified dmisteinbergite, the rare trigonal polymorph of CaAl2Si2O8, for the first time in
high-grade metamorphic rocks. Dmisteinbergite occurs as a crystallization product of silicate …
high-grade metamorphic rocks. Dmisteinbergite occurs as a crystallization product of silicate …