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 2022-01-01 to 2026-01-01.)
ArticleCitations
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Thermal pulse induced by emplacement of Ramba leucogranites in southern Tibet29
Petrochronology of polygenetic white micas (Naxos, Greece)27
Hydration of mafic crustal rocks at high temperature during brittle‐viscous deformation along a strike‐slip plate boundary27
Significance of selective crystal entrainment and differential crystal‐melt separation in petrogenesis of granites from the Tongbai orogen25
Low‐grade prehnite‐pumpellyite facies metamorphism and metasomatism in basement rocks adjacent to the Permian Oslo rift: The importance of displacive reactions25
Pressure–temperature paths of tectonic blocks in mélange: Recording thermal evolution of a subduction channel at an initial stage of subduction20
Constraining the P–T path of (U)HP rocks with reaction overstepping during subduction; example from the Western Gneiss Region (Norway)19
A buried gneiss dome in the northern Gawler Craton: The record of early Mesoproterozoic (ca. 1600–1560 Ma) extension in southern Proterozoic Australia18
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Carboniferous Barrovian to Permian Buchan‐type metamorphic cycles in the Mongolian Altai Zone: Implication for pressure cycles in accretionary orogens16
Polyphase tectonic reworking of serpentinites and chlorite‐tremolite‐talc rocks (SW Spain) from the subduction forearc to intracontinental emplacement15
The Structure and P–T–t–d Evolution of the Saxothuringian/Brunovistulian Variscan Boundary Zone in the Bohemian Massif (Czech Republic, Poland)14
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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 Asia14
The Piedmont Zone From the Western Alps (Italy): New Insights From High‐Pressure Ophiolitic Metasediments in the Soana Valley13
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Thermodynamic constraints on the composition of orogenically thickened lower crust12
Redistribution of heat‐producing elements during melting of Archean crust11
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Effects of Fe3+ in sillimanite on mineral stabilities and parageneses in ultrahigh‐temperature metapelites11
Disruption of a high‐pressure unit during exhumation: Example of the Cycladic Blueschist unit (Thera, Ios and Naxos islands, Greece)11
Comparison of Water Contents Between Ultrahigh‐Pressure Oceanic and Continental Eclogites From the North Qaidam Orogen11
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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 crust10
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The origin and compositions of melt inclusions in an Al2SiO5‐free paragneiss from the Namche Barwa Complex in the Eastern Himalayan Syntaxis9
Trace‐element heterogeneity in rutile linked to dislocation structures: Implications for Zr‐in‐rutile geothermometry9
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Polyphase Metamorphism of the Northern Rae Craton (Baffin Island, Arctic Canada) and Trace Element Behaviour in Monazite: Insights From Phase Equilibria Modelling and Geochronology9
Probing intra‐oceanic subduction infancy in ancient orogenic belts: Example from Chinese South Tianshan9
Isochemical metamorphism origin of the newly discovered Baqing jadeitoid, eastern‐central Tibet, China9
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Kinetics and pulses of zircon growth in migmatites beneath a volcanic arc: An example from the high‐T Ryoke Complex, southwest Japan9
Implications of garnet nucleation overstepping for the P–T evolution of the Lesser Himalayan Sequence of central Nepal8
The temporal evolution of subduction initiation in the Samail ophiolite: High‐precision U–Pb zircon petrochronology of the metamorphic sole8
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Polyphase Deformation During Prolonged High‐Temperature, Low‐Pressure Metamorphism: An Example From the Namibfontein‐Vergenoeg Migmatite Domes, Central Zone, Damara Belt, Namibia7
Thorium zoning in monazite: A case study from the Ivrea–Verbano zone, NW Italy7
Deviation between quartz‐in‐garnet elastic geobarometry and equilibrium‐based pressure–temperature modelling in Barrovian metamorphic rocks7
Multi‐Stage Growth of Kyanite in Migmatites Interpreted by Integrating Forward Thermodynamic Modelling and Trace Element Signature7
Isothermal compression of an eclogite from the Western Gneiss Region (Norway)7
Out‐of‐Sequence Nucleation in a Blueschist From Syros, Greece7
Polymetamorphism during the Grenvillian Orogeny in SE Ontario: Results from trace element mapping, in situ geochronology, and diffusion geospeedometry7
Multi‐mineral petrochronology on a high‐pressure mafic granulite reveals short‐lived high‐temperature metamorphism in the North China Craton7
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
Experimental Replacement of Zircon by Melt‐Mediated Coupled Dissolution‐Precipitation Causes Dispersion in U–Pb Ages6
Metamorphic and chronological constraints on the early Paleozoic tectono‐thermal evolution of the Olkhon Terrane, southern Siberia6
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Carboniferous–Triassic tectonic and thermal evolution of the middle crust section of the Dervio–Olgiasca Zone (Southern Alps)5
Location, Location, Location: Monazite Behaviour During UHT Metamorphism and Melt Crystallization5
Tectonothermal Evolution of the NW Wyoming Province: Insights From Coupled Garnet Lu‐Hf and Sm‐Nd Geochronology5
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Deformation‐induced graphitization and muscovite recrystallization in a ductile fault zone5
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Exhumation of deep continental crust in a transpressive regime: The example of Variscan eclogites from the Aiguilles‐Rouges massif (Western Alps)5
Orogen‐scale uniformity of recorded granulite facies conditions due to thermal buffering and melt retention5
Vanishing Evidence of Ultrahigh‐Pressure Metamorphism: A Case Study of the Rhodope Metamorphic Complex, Greece4
Eclogite thermobarometry: The consistency between conventional thermobarometry and forward phase‐equilibrium modelling4
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
Pressure and Temperature Estimation in Greenschist‐Facies Metapelites: An Example From the Variscan Belt in Sardinia4
Interplay Between Mechanical and Petrochemical Models on the Fluid Extraction From Subduction Zones4
Geothermometric constraints on the thermal architecture, metamorphism, and exhumation of the Northern Range, Trinidad4
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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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Retentiveness of rare earth elements in garnet with implications for garnet Lu‐Hf chronology4
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, Pakistan4
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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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A New UHP‐HP Tectono‐Metamorphic Architecture for the Southern Dora‐Maira Massif Nappe Stack (Western Alps) Based on Petrological and Microstructural Evidence4
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Zircon (Re)crystallization During Metamorphism: Zircon Paragenesis in the Papua New Guinea Coesite Eclogite Revisited3
Archean ultrahigh temperature event in the northwestern Superior Province, Canada: Metamorphic evolution and tectonic implications of the Pikwitonei Granulite Domain3
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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
To be or not to be Alpine: New petrological constraints on the metamorphism of the Chenaillet Ophiolite (Western Alps)3
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Thermodynamic and Kinetic Controls on the Growth of Metapelitic Garnet in the Danba Dome (SW China): Insights From Microstructure, Element Mapping and Thermodynamic Modelling3
Garnet growth and mineral geochronology constrains the diachronous Neoproterozoic convergent evolution of the southern Dom Feliciano Belt, Uruguay3
40Ar/39Ar dates controlled by white mica deformation and strain localization: Insights from comparing in situ laser ablation and single‐grain fusion techniques3
Discrimination of thermodynamic and kinetic contributions to the heavy rare earth element patterns in metamorphic garnet3
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Contact Metamorphism of Pelitic Rocks Constrains the Depth of Emplacement of the Re di Castello Intrusion (Adamello Batholith, Italy)3
P–T–t–D records of Early Palaeozoic Andean‐type shortening of a hot active margin: The Dunhuang block in NW China3
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Heat sources for Variscan high‐temperature–low‐pressure metamorphism: Petrochronological constraints from the Trois Seigneurs massif, French Pyrenees3
Metamorphic evolution and geological significance of Early Palaeozoic high‐pressure granulites from the East Kunlun (NW China)3
Influence of high‐strain deformation on major element mobility in garnet: Nanoscale evidence from atom probe tomography3
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Alpine subduction zone metamorphism in the Palaeozoic successions of the Monti Romani (Northern Apennines, Italy)3
Ultrahigh‐Temperature Metamorphism and Near‐Isobaric Cooling of Garnet‐Orthopyroxene Granulite Xenoliths in the Sancheong Anorthosite, Yeongnam Massif, Korea2
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Allanite U–Pb dating places new constraints on the high‐pressure to high‐temperature evolution of the deep Himalayan crust2
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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
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Archean Polymetamorphism in the Central Dharwar Craton, Southern India2
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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Fluid or Melt? Distinguishing Syn‐Deformational Interaction Pathways1
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Prograde zircon growth in migmatites1
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The inhibited response of accessory minerals during high‐temperature reworking1
Zircon Coupled Dissolution–Precipitation Replacement During Melt–Rock Interaction Modifies Chemical Signatures Resulting in Misleading Ages1
Coeval formation and exhumation of metamorphic sole and ophiolite in the Saga ophiolitic mélange: Insights into subduction initiation of the Neo‐Tethys1
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Low temperature eclogite facies rocks discovered in the Eastern Himalayan Syntaxis: Poly‐cyclic metamorphic evolution and implications1
Dehydration‐driven deformation of eclogite: Interplay between fluid discharge and rheology1
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Partial melting and reaction along deformation features in plagioclase1
Eclogite with biotite porphyroblasts—Which conditions are responsible for their formation? An example from the northern Fleur‐de‐Lys Supergroup, Newfoundland, Canada1
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