Journal of Metamorphic Geology

Papers
(The median citation count of Journal of Metamorphic Geology is 1. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2021-09-01 to 2025-09-01.)
ArticleCitations
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Hydration of mafic crustal rocks at high temperature during brittle‐viscous deformation along a strike‐slip plate boundary25
Petrochronology of polygenetic white micas (Naxos, Greece)24
Thermal pulse induced by emplacement of Ramba leucogranites in southern Tibet24
A thermodynamic model for feldspars in KAlSi3O8−NaAlSi3O8−CaAl2Si2O8 for mineral equilibrium calculations24
Constraining the P–T path of (U)HP rocks with reaction overstepping during subduction; example from the Western Gneiss Region (Norway)23
Significance of selective crystal entrainment and differential crystal‐melt separation in petrogenesis of granites from the Tongbai orogen22
Pressure–temperature paths of tectonic blocks in mélange: Recording thermal evolution of a subduction channel at an initial stage of subduction21
A buried gneiss dome in the northern Gawler Craton: The record of early Mesoproterozoic (ca. 1600–1560 Ma) extension in southern Proterozoic Australia18
Low‐grade prehnite‐pumpellyite facies metamorphism and metasomatism in basement rocks adjacent to the Permian Oslo rift: The importance of displacive reactions18
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The Structure and P–T–t–d Evolution of the Saxothuringian/Brunovistulian Variscan Boundary Zone in the Bohemian Massif (Czech Republic, Poland)16
Repeated metamorphism in the pelitic granulites of the Hidaka metamorphic belt, Hokkaido, Japan: Implications for the formation of the present‐day trench‐arc‐basin system in NE Asia16
Polyphase tectonic reworking of serpentinites and chlorite‐tremolite‐talc rocks (SW Spain) from the subduction forearc to intracontinental emplacement15
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Thermodynamic constraints on the composition of orogenically thickened lower crust14
Carboniferous Barrovian to Permian Buchan‐type metamorphic cycles in the Mongolian Altai Zone: Implication for pressure cycles in accretionary orogens14
Redistribution of heat‐producing elements during melting of Archean crust13
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Amalgamation of the Ryoke and Sanbagawa metamorphic belts at the subduction interface: New insights from the Kashio mylonite along the Median Tectonic Line, Nagano, Japan12
Effects of Fe3+ in sillimanite on mineral stabilities and parageneses in ultrahigh‐temperature metapelites12
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Disruption of a high‐pressure unit during exhumation: Example of the Cycladic Blueschist unit (Thera, Ios and Naxos islands, Greece)11
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Ultrahigh thermal gradient granulites in the Narryer Terrane, Yilgarn Craton, Western Australia, provide a window into the composition and formation of Archean lower crust11
Comparison of Water Contents Between Ultrahigh‐Pressure Oceanic and Continental Eclogites From the North Qaidam Orogen11
Polyphase Metamorphism of the Northern Rae Craton (Baffin Island, Arctic Canada) and Trace Element Behaviour in Monazite: Insights From Phase Equilibria Modelling and Geochronology10
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Ultrahigh‐temperature Palaeoproterozoic rocks in the Neoproterozoic Borborema Province, implications for São Francisco Craton dispersion in NE Brazil9
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The slab–mantle wedge interface of an incipient subduction zone: Insights from the PTD evolution and petrological characteristics of the Dalrymple Amphibolite, Palawan Ophiolite9
Isochemical metamorphism origin of the newly discovered Baqing jadeitoid, eastern‐central Tibet, China9
Kinetics and pulses of zircon growth in migmatites beneath a volcanic arc: An example from the high‐T Ryoke Complex, southwest Japan9
The origin and compositions of melt inclusions in an Al2SiO5‐free paragneiss from the Namche Barwa Complex in the Eastern Himalayan Syntaxis9
Isothermal compression of an eclogite from the Western Gneiss Region (Norway)8
Multi‐Stage Growth of Kyanite in Migmatites Interpreted by Integrating Forward Thermodynamic Modelling and Trace Element Signature8
Probing the history of ultra‐high temperature metamorphism through rare earth element diffusion in zircon8
Probing intra‐oceanic subduction infancy in ancient orogenic belts: Example from Chinese South Tianshan8
Multi‐mineral petrochronology on a high‐pressure mafic granulite reveals short‐lived high‐temperature metamorphism in the North China Craton8
Trace‐element heterogeneity in rutile linked to dislocation structures: Implications for Zr‐in‐rutile geothermometry8
Implications of garnet nucleation overstepping for the P–T evolution of the Lesser Himalayan Sequence of central Nepal8
Polymetamorphism during the Grenvillian Orogeny in SE Ontario: Results from trace element mapping, in situ geochronology, and diffusion geospeedometry8
The temporal evolution of subduction initiation in the Samail ophiolite: High‐precision U–Pb zircon petrochronology of the metamorphic sole8
Multi‐stage metamorphic history of the Oki gneisses in Japan: Implications for Paleoproterozoic metamorphism and tectonic correlations in northeastern Asia8
Metamorphic and chronological constraints on the early Paleozoic tectono‐thermal evolution of the Olkhon Terrane, southern Siberia7
Polyphase Deformation During Prolonged High‐Temperature, Low‐Pressure Metamorphism: An Example From the Namibfontein‐Vergenoeg Migmatite Domes, Central Zone, Damara Belt, Namibia7
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Thorium zoning in monazite: A case study from the Ivrea–Verbano zone, NW Italy7
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Paleoproterozoic ultrahigh‐temperature metamorphism in the Alxa Block, the Khondalite Belt, North China Craton: Petrology and phase equilibria of quartz‐absent corundum‐bearing pelitic granulites6
Deviation between quartz‐in‐garnet elastic geobarometry and equilibrium‐based pressure–temperature modelling in Barrovian metamorphic rocks6
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Experimental Replacement of Zircon by Melt‐Mediated Coupled Dissolution‐Precipitation Causes Dispersion in U–Pb Ages6
Out‐of‐Sequence Nucleation in a Blueschist From Syros, Greece6
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Cold deep subduction of Indian continental crust and release of ultrahigh‐pressure fluid during initial exhumation: Insights from coesite‐bearing eclogite‐vein systems in Kaghan Valley, Pakistan5
A New UHP‐HP Tectono‐Metamorphic Architecture for the Southern Dora‐Maira Massif Nappe Stack (Western Alps) Based on Petrological and Microstructural Evidence5
Deformation‐induced graphitization and muscovite recrystallization in a ductile fault zone5
Exhumation of deep continental crust in a transpressive regime: The example of Variscan eclogites from the Aiguilles‐Rouges massif (Western Alps)5
Retentiveness of rare earth elements in garnet with implications for garnet Lu‐Hf chronology5
Orogen‐scale uniformity of recorded granulite facies conditions due to thermal buffering and melt retention5
Carboniferous–Triassic tectonic and thermal evolution of the middle crust section of the Dervio–Olgiasca Zone (Southern Alps)5
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Geothermometric constraints on the thermal architecture, metamorphism, and exhumation of the Northern Range, Trinidad5
Tectonothermal Evolution of the NW Wyoming Province: Insights From Coupled Garnet Lu‐Hf and Sm‐Nd Geochronology5
An extensive record of orogenesis recorded in a Madagascar granulite4
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Pressure and Temperature Estimation in Greenschist‐Facies Metapelites: An Example From the Variscan Belt in Sardinia4
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Eclogite thermobarometry: The consistency between conventional thermobarometry and forward phase‐equilibrium modelling4
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Ultrahigh temperature metamorphism and isobaric cooling of Neoarchean ultramafic‐mafic granulites in the southern granulite terrain, India: Phase equilibrium modelling and SHRIMP zircon U–Pb dating4
Assessing the importance of H2O content in the tectono‐metamorphic evolution of shear zones: A case study from the Dora‐Maira Massif (Western Alps)4
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High‐pressure granulite facies re‐equilibration and zoisite–biotite dehydration melting during decompression of an ultrahigh‐pressure garnet clinopyroxenite from the island of Fjørtoft, Norway4
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New constraints on the tectonometamorphic evolution of the Erzgebirge orogenic wedge (Saxothuringian Domain, Bohemian Massif)3
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Contact Metamorphism of Pelitic Rocks Constrains the Depth of Emplacement of the Re di Castello Intrusion (Adamello Batholith, Italy)3
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Influence of high‐strain deformation on major element mobility in garnet: Nanoscale evidence from atom probe tomography3
Thermodynamic and Kinetic Controls on the Growth of Metapelitic Garnet in the Danba Dome (SW China): Insights From Microstructure, Element Mapping and Thermodynamic Modelling3
Alpine subduction zone metamorphism in the Palaeozoic successions of the Monti Romani (Northern Apennines, Italy)3
To be or not to be Alpine: New petrological constraints on the metamorphism of the Chenaillet Ophiolite (Western Alps)3
Discrimination of thermodynamic and kinetic contributions to the heavy rare earth element patterns in metamorphic garnet3
40Ar/39Ar dates controlled by white mica deformation and strain localization: Insights from comparing in situ laser ablation and single‐grain fusion techniques3
Heat sources for Variscan high‐temperature–low‐pressure metamorphism: Petrochronological constraints from the Trois Seigneurs massif, French Pyrenees3
Archean ultrahigh temperature event in the northwestern Superior Province, Canada: Metamorphic evolution and tectonic implications of the Pikwitonei Granulite Domain3
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P–T–t–D records of Early Palaeozoic Andean‐type shortening of a hot active margin: The Dunhuang block in NW China3
Tectonic Setting and Evolution of Anatectic Melt Composition During Prograde Metamorphism up to UHT Metamorphism: Constraints From P–T–t–Melting Path From Rundvågshetta, Lützow–Holm Complex, Ea3
Metamorphic evolution and geological significance of Early Palaeozoic high‐pressure granulites from the East Kunlun (NW China)3
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Late Famatinian (440–410 Ma) overprint of Grenvillian metamorphism in Grt‐St schists from the Sierra de Maz (Argentina): Phase equilibrium modelling, geochronology, and tectonic significance2
Pressure–temperature–time–deformation (P–T–t–d) path for Devonian forearc deposits in the Imjingang Belt, South Korea: Implications for Permian–Triassic collisional orogenesis on the eastern ma2
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Allanite U–Pb dating places new constraints on the high‐pressure to high‐temperature evolution of the deep Himalayan crust2
Prograde zircon growth in migmatites2
The inhibited response of accessory minerals during high‐temperature reworking2
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Garnet growth and mineral geochronology constrains the diachronous Neoproterozoic convergent evolution of the southern Dom Feliciano Belt, Uruguay2
Archean Polymetamorphism in the Central Dharwar Craton, Southern India2
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Partial melting and reaction along deformation features in plagioclase2
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Zircon (Re)crystallization During Metamorphism: Zircon Paragenesis in the Papua New Guinea Coesite Eclogite Revisited2
Plate Interface Shear Zone in the Sanbagawa Metamorphic Belt, Constrained by RSCM Thermometry, U–Pb Zircon Dating and Phase Equilibria Modelling in the Sarutagawa Region, Central Shikoku, Japan2
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Coeval formation and exhumation of metamorphic sole and ophiolite in the Saga ophiolitic mélange: Insights into subduction initiation of the Neo‐Tethys2
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Consistent garnet Lu–Hf and Sm–Nd ages indicate short‐lived high‐pressure metamorphism and rapid subduction in oceanic subduction belt: An example from the Changning–Menglian orogenic belt, southeaste1
Preservation of mantle heterogeneities and serpentinization signature during antigorite dehydration: The example of the Bergell contact aureole1
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Low temperature eclogite facies rocks discovered in the Eastern Himalayan Syntaxis: Poly‐cyclic metamorphic evolution and implications1
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Zircon Coupled Dissolution–Precipitation Replacement During Melt–Rock Interaction Modifies Chemical Signatures Resulting in Misleading Ages1
Eclogite with biotite porphyroblasts—Which conditions are responsible for their formation? An example from the northern Fleur‐de‐Lys Supergroup, Newfoundland, Canada1
Fluid‐driven transformation of blueschist to vein eclogite during the Early Eocene in a subducted sliver of continental crust (Monte Emilius, Italian Western Alps)1
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Repeated Caledonian burial and ultrafast cooling and exhumation of high‐pressure granulite facies rocks from the Blåhø Nappe on the island of Fjørtoft, Western Gneiss Region, Norway1
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Dehydration‐driven deformation of eclogite: Interplay between fluid discharge and rheology1
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