Journal of Metamorphic Geology

Papers
(The median citation count of Journal of Metamorphic Geology is 0. 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 2021-04-01 to 2025-04-01.)
ArticleCitations
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Implications of garnet nucleation overstepping for the P–T evolution of the Lesser Himalayan Sequence of central Nepal41
Thermal pulse induced by emplacement of Ramba leucogranites in southern Tibet27
Pressure–temperature–time evolution of subducted crust revealed by complex garnet zoning (Theodul Glacier Unit, Switzerland)22
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Fluid‐driven transformation of blueschist to vein eclogite during the Early Eocene in a subducted sliver of continental crust (Monte Emilius, Italian Western Alps)21
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Significance of selective crystal entrainment and differential crystal‐melt separation in petrogenesis of granites from the Tongbai orogen20
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A Prograde Dual‐Segmented Geotherm for (Retro‐) Eclogite From Western Dabie and Implications for Maximum Decoupling Depths During Continental Subduction20
Bulk inclusion micro‐zircon U–Pb geochronology: A new tool to date low‐grade metamorphism19
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Multi‐mineral petrochronology on a high‐pressure mafic granulite reveals short‐lived high‐temperature metamorphism in the North China Craton17
Polymetamorphism during the Grenvillian Orogeny in SE Ontario: Results from trace element mapping, in situ geochronology, and diffusion geospeedometry17
Dehydration‐driven deformation of eclogite: Interplay between fluid discharge and rheology17
The inhibited response of accessory minerals during high‐temperature reworking15
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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 China14
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Low‐grade prehnite‐pumpellyite facies metamorphism and metasomatism in basement rocks adjacent to the Permian Oslo rift: The importance of displacive reactions14
A buried gneiss dome in the northern Gawler Craton: The record of early Mesoproterozoic (ca. 1600–1560 Ma) extension in southern Proterozoic Australia14
Eclogite with biotite porphyroblasts—Which conditions are responsible for their formation? An example from the northern Fleur‐de‐Lys Supergroup, Newfoundland, Canada14
Alpine subduction zone metamorphism in the Palaeozoic successions of the Monti Romani (Northern Apennines, Italy)13
Partial melting mechanisms of peraluminous felsic magmatism in a collisional orogen: An example from the Khondalite belt, North China craton13
Pressure–Temperature–Time Evolution of a Polymetamorphic Paragneiss With Pseudomorphs After Jadeite From the HP–UHP Gneiss‐Eclogite Unit of the Variscan Erzgebirge Crystalline Complex, Germany12
Hydration of mafic crustal rocks at high temperature during brittle‐viscous deformation along a strike‐slip plate boundary12
Isothermal compression of an eclogite from the Western Gneiss Region (Norway)12
A window into an older orogenic cycle: P–T conditions and timing of the pre‐Alpine history of the Dora‐Maira Massif (Western Alps)12
Zircon Coupled Dissolution–Precipitation Replacement During Melt–Rock Interaction Modifies Chemical Signatures Resulting in Misleading Ages11
Gabbroic eclogites formed during rapid and cold subduction of the Paleo‐Tethys oceanic lithosphere in the Changning–Menglian orogenic belt, southeastern Tibetan plateau10
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Constraining the P–T path of (U)HP rocks with reaction overstepping during subduction; example from the Western Gneiss Region (Norway)10
Thorium zoning in monazite: A case study from the Ivrea–Verbano zone, NW Italy10
Combined phase diagram modelling and quartz‐in‐garnet barometry of HP metapelites from the Kamieniec Metamorphic Belt (NE Bohemian Massif)9
Low temperature eclogite facies rocks discovered in the Eastern Himalayan Syntaxis: Poly‐cyclic metamorphic evolution and implications9
Metamorphic transformation rate over large spatial and temporal scales constrained by geophysical data and coupled modelling9
Partially open grain and phase boundaries as fluid pathways in metamorphic and magmatic rocks9
Constraints on the Palaeoproterozoic tectono‐metamorphic evolution of the Lewisian Gneiss Complex, NW Scotland: Implications for Nuna assembly9
To be or not to be Alpine: New petrological constraints on the metamorphism of the Chenaillet Ophiolite (Western Alps)8
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Multi‐Stage Growth of Kyanite in Migmatites Interpreted by Integrating Forward Thermodynamic Modelling and Trace Element Signature8
Mechanisms and durations of metamorphic garnet crystallization in the lower nappes of the Caledonian Kalak Nappe Complex, Arctic Norway8
A thermodynamic model for feldspars in KAlSi3O8−NaAlSi3O8−CaAl2Si2O8 for mineral equilibrium calculations8
Pressure–temperature paths of tectonic blocks in mélange: Recording thermal evolution of a subduction channel at an initial stage of subduction8
Carboniferous high‐P metamorphism and deformation in the Belledonne Massif (Western Alps)8
Petrochronology of polygenetic white micas (Naxos, Greece)8
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Garnet, zircon, and monazite age and REE signatures in (ultra)high‐temperature and high‐pressure rocks: Examples from the Caledonides and the Pamir7
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The tempo and conditions of metamorphism during magmatism, southern Coast Mountains batholith, British Columbia, Canada7
Incompatibility between serpentinization and epidote formation in the lower oceanic crust: Evidence from the Oman Drilling Project6
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Garnet growth and mineral geochronology constrains the diachronous Neoproterozoic convergent evolution of the southern Dom Feliciano Belt, Uruguay6
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, Norway6
A rutile and titanite record of subduction fluids: Integrated oxygen isotope and trace element analyses in Franciscan high‐pressure rocks6
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Experimental Replacement of Zircon by Melt‐Mediated Coupled Dissolution‐Precipitation Causes Dispersion in U–Pb Ages6
Devonian Andean‐type convergence in the southern Dunhuang block (NW China): Petro‐structural, metamorphic P–T and geochronological constraints6
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Formation of low‐pressure reaction textures during near‐isothermal exhumation of hot orogenic crust (Bohemian Massif, Austria)5
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Metasomatism of the continental crust and its impact on surface uplift: Insights from reactive‐transport modelling5
Phase Equilibria Analysis for Metacarbonate With Applications to Zoned Calc‐Silicate Aureoles4
Was cratonic Asia deeply subducted beneath the Pamir? Evidence from P–T conditions and tectonic affinities of Cenozoic Pamir crustal xenoliths4
Diachronous collision in the Seve Nappe Complex: Evidence from Lu–Hf geochronology of eclogites (Norrbotten, North Sweden)4
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 Asia4
Deviation between quartz‐in‐garnet elastic geobarometry and equilibrium‐based pressure–temperature modelling in Barrovian metamorphic rocks4
Pressure–temperature–time constraints on gneiss dome formation in an intracontinental orogen4
The Structure and P–T–t–d Evolution of the Saxothuringian/Brunovistulian Variscan Boundary Zone in the Bohemian Massif (Czech Republic, Poland)4
P–T–t conditions of Early Palaeozoic low‐P high‐T granulite facies metamorphism in the southern Truong Son Belt, Central Vietnam4
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Paleoproterozoic ultrahigh‐temperature mafic granulites with a high‐pressure prograde path from the Alxa Block: Implications on the tectonic evolution of the Khondalite Belt, North China Craton4
Multistage metamorphism of eclogite in the South Altyn HP–UHP belt, Northwest China: Deep subduction and exhumation process of continental crust3
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, southeaste3
Strengths and limitations of in situ U–Pb titanite petrochronology in polymetamorphic rocks: An example from western Maine, USA3
A Mechanistic Look at the Amphibolitization of Mafic Crust: Insights From the Kråkeneset Gabbro Body, Western Gneiss Region, Norway3
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Contact Metamorphism of Pelitic Rocks Constrains the Depth of Emplacement of the Re di Castello Intrusion (Adamello Batholith, Italy)3
Alpine tectono‐metamorphic evolution of the Corsica basement3
Metamorphic and chronological constraints on the early Paleozoic tectono‐thermal evolution of the Olkhon Terrane, southern Siberia3
Modification of the isotopic and geochemical compositions of accessory minerals controlled by microstructural setting3
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Carboniferous Barrovian to Permian Buchan‐type metamorphic cycles in the Mongolian Altai Zone: Implication for pressure cycles in accretionary orogens3
Polyphase tectonic reworking of serpentinites and chlorite‐tremolite‐talc rocks (SW Spain) from the subduction forearc to intracontinental emplacement3
GeoPS: An interactive visual computing tool for thermodynamic modelling of phase equilibria2
Paleoproterozoic ultrahigh‐temperature metamorphism in the Alxa Block, the Khondalite Belt, North China Craton: Petrology and phase equilibria of quartz‐absent corundum‐bearing pelitic granulites2
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The origin of calcite in calc‐silicate rocks from the Kokchetav ultrahigh‐pressure metamorphic complex2
Preservation of mantle heterogeneities and serpentinization signature during antigorite dehydration: The example of the Bergell contact aureole2
Discrimination of thermodynamic and kinetic contributions to the heavy rare earth element patterns in metamorphic garnet2
Metamorphic evolution and geological significance of Early Palaeozoic high‐pressure granulites from the East Kunlun (NW China)2
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Monazite petrochronology of polymetamorphic granulite‐facies rocks of the Larsemann Hills, Prydz Bay, East Antarctica2
Late Neoproterozoic–Cambrian eclogites and high‐pressure granulites in the Central Qilian terrane (China) record the earliest subduction of Proto‐Tethyan Ocean in the eastern Tethysides2
Cold Deep Over Hot Shallow Crust: A Peculiar Metamorphic Architecture in the Neoarchean Metasedimentary Pontiac Subprovince, Superior Craton (Canada)2
Thermodynamic constraints on the composition of orogenically thickened lower crust2
Formation of multistage garnet grains by fragmentation and overgrowth constrained by microchemical and microstructural mapping2
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Metamorphic PTtd evolution of the Mesoproterozoic Pur‐Banera supracrustal belt, Aravalli Craton, northwestern India: Insights from phase equilibria modelling and zircon–2
Kyanite and Cordierite‐Andalusite occurrences in parts of Barrow's Staurolite zones – The effects of high ferric iron2
Effects of Fe3+ in sillimanite on mineral stabilities and parageneses in ultrahigh‐temperature metapelites1
Protracted eclogite‐facies metamorphism of the Dulan area, North Qaidam ultrahigh‐pressure terrane: Insights on zircon growth during continental subduction and collision1
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Deciphering the tectonometamorphic history of subducted metapelites using quartz‐in‐garnet and Ti‐in‐quartz (QuiG–TiQ) geothermobarometry—A key for understanding burial in the Scandinavian Caledonides1
Carboniferous–Triassic tectonic and thermal evolution of the middle crust section of the Dervio–Olgiasca Zone (Southern Alps)1
Disruption of a high‐pressure unit during exhumation: Example of the Cycladic Blueschist unit (Thera, Ios and Naxos islands, Greece)1
A diachronous record of metamorphism in metapelites of the Western Gneiss Region, Norway1
Barrovian and Buchan metamorphic series in the Chinese Altai:P–T–t–D evolution and tectonic implications1
Petrochronologic constraints on inverted metamorphism, terrane accretion, thrust stacking, and ductile flow in the Gneiss Dome belt, northern Appalachian orogen1
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Redistribution of heat‐producing elements during melting of Archean crust1
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Complex geochronological record of an emblematic Variscan eclogite (Haut‐Allier, French Massif Central)1
Melt–Rock Interaction Experiments Reveal Rapid Microstructural and Chemical Changes at Lower Crustal Conditions0
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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‐Tethys0
Ultrahigh‐temperature Palaeoproterozoic rocks in the Neoproterozoic Borborema Province, implications for São Francisco Craton dispersion in NE Brazil0
Evidence of High‐Pressure Metamorphism Along the Mahanadi Shear Zone in the Eastern Ghats Province, Eastern India: Implications on Tectonics and Continental Assembly Involving India and East Antarctic0
Thermal structure in subducted units from continental Moho depths in a palaeo subduction zone, the Asemigawa region of the Sanbagawa metamorphic belt, SW Japan0
From microanalysis to supercontinents: Insights from the Rio Apa Terrane into the Mesoproterozoic SW Amazonian Craton evolution during Rodinia assembly0
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Calculated phase equilibria for high‐pressure serpentinites and compositionally related rocks close to the MgO–Al2O3–SiO2–H2O (MASH) system0
H2O in omphacite of quartz and coesite eclogite from Erzgebirge and Fichtelgebirge, Germany0
Archean Polymetamorphism in the Central Dharwar Craton, Southern India0
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New constraints on the tectonometamorphic evolution of the Erzgebirge orogenic wedge (Saxothuringian Domain, Bohemian Massif)0
HP–UHT granulites in the East Kunlun Orogen, NW China: Constraints on the transition from compression to extension in an arc setting of the Proto‐Tethys Ocean0
Chromium in minerals as tracer of the polycyclic evolution of eclogite and related metabasite from the Pohorje Mountains, Slovenian Eastern Alps0
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 ma0
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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 significance0
Origin of Erzgebirge ultrahigh‐pressure garnetite: Formation from a basaltic protolith by serpentinization‐assisted metasomatism?0
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Phase equilibria and microstructural constraints on the high‐T building of the Kohistan island arc: The Jijal garnet granulites, northern Pakistan0
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40Ar/39Ar dates controlled by white mica deformation and strain localization: Insights from comparing in situ laser ablation and single‐grain fusion techniques0
Geothermometric constraints on the thermal architecture, metamorphism, and exhumation of the Northern Range, Trinidad0
Pressure–temperature evolution of the basement and cover sequences on Ios, Greece: Evidence for subduction of the Hercynian basement0
An extensive record of orogenesis recorded in a Madagascar granulite0
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Eclogite thermobarometry: The consistency between conventional thermobarometry and forward phase‐equilibrium modelling0
The controls on the thermal evolution of continental mountain ranges0
Garnet crystallization mechanisms and localized polymetamorphism in the southwestern Meguma Terrane, Nova Scotia, Canada0
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Pronounced and rapid exhumation of the Connecticut Valley Trough revealed through quartz in garnet Raman barometry and diffusion modelling of garnet dissolution–reprecipitation reactions0
High‐pressure granulite facies re‐equilibration and zoisite–biotite dehydration melting during decompression of an ultrahigh‐pressure garnet clinopyroxenite from the island of Fjørtoft, Norway0
Pressure and Temperature Estimation in Greenschist‐Facies Metapelites: An Example From the Variscan Belt in Sardinia0
Trace‐element heterogeneity in rutile linked to dislocation structures: Implications for Zr‐in‐rutile geothermometry0
Hydrous shear zones are sites of melt transfer in the lower arc crust: A case study from Fiordland, New Zealand0
Growth of kyanite and Fe‐Mg chloritoid in Fe2O3‐rich high‐pressure–low‐temperature metapelites and metapsammites: A case study from the Massa Unit (Alpi Apuane, Italy)0
Trapped K‐feldspar phenocrysts as a signature of melt migration pathways within active high‐strain zones0
Probing intra‐oceanic subduction infancy in ancient orogenic belts: Example from Chinese South Tianshan0
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Self‐induced incipient ‘eclogitization’ of metagranitoids at closed‐system conditions0
Abiotic passive nitrogen and methane enrichment during exhumation of subducted rocks: Primary multiphase fluid inclusions in high‐pressure rocks from the Cabo Ortegal Complex, NW Spain0
Testing the equilibrium model: An example from the Caledonian Kalak Nappe Complex (Finnmark, Arctic Norway)0
Paleoarchean metamorphism in the Acasta Gneiss Complex: Constraints from phase equilibrium modelling and in situ garnet Lu–Hf geochronology0
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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, Japan0
The temporal evolution of subduction initiation in the Samail ophiolite: High‐precision U–Pb zircon petrochronology of the metamorphic sole0
Deformation‐induced graphitization and muscovite recrystallization in a ductile fault zone0
Partial melting and reaction along deformation features in plagioclase0
A wealth of P–T–t information from metasediments in the HP–UHP terrane of the Pohorje Mountains, Slovenia, elucidates the evolution of the Eastern Alps0
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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, Japan0
Petrochronology of High‐Pressure Veins Reveals the Evolution of Fluid Sources in Subducted Oceanic Crust (Rocciavrè Eclogites, W. Alps)0
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Late Variscan (315 Ma) subduction or deceptive zircon REE patterns and U–Pb dates from migmatite‐hosted eclogites? (Montagne Noire, France)0
Pattern and source of unusually high‐temperature metamorphism in an Eocene forearc recorded by the Pacific Rim Terrane, British Columbia, Canada0
Tectonic erosion and deep subduction in Central Tibet: Evidence from the discovery of retrograde eclogites in the Amdo microcontinent0
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HTLP metamorphism and fluid‐fluxed melting during multistage anatexis of continental crust (N Sardinia, Italy)0
Orogen‐scale uniformity of recorded granulite facies conditions due to thermal buffering and melt retention0
Allanite U–Pb dating places new constraints on the high‐pressure to high‐temperature evolution of the deep Himalayan crust0
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 dating0
Reconstructing the metamorphic evolution of the Araçuaí orogen (SE Brazil) using in situ U–Pb garnet dating and PT modelling0
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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)0
Petrogenesis of the Scapolite‐Bearing Kongurblak Shear Zone, Chinese Southwestern Tianshan: Implications for Rock‐Buffered Fluid Flow Migration During Orogeny0
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Constraining the process of intracontinental subduction in the Austroalpine Nappes: Implications from petrology and Lu‐Hf geochronology of eclogites0
Peritectic minerals record partial melting of the deeply subducted continental crust in the Sulu orogen0
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Predicting and explaining crystallographic orientation relationships of exsolved precipitates in garnet using the edge‐to‐edge matching model0
Mike Brown Annual Early Career JMG Research Paper Prize and Douglas Robinson JMG annual reviewer award0
The slab–mantle wedge interface of an incipient subduction zone: Insights from the PTD evolution and petrological characteristics of the Dalrymple Amphibolite, Palawan Ophiolite0
Deep subduction, melting, and fast cooling of metapelites from the Cima Lunga Unit, Central Alps0
Archean ultrahigh temperature event in the northwestern Superior Province, Canada: Metamorphic evolution and tectonic implications of the Pikwitonei Granulite Domain0
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Retentiveness of rare earth elements in garnet with implications for garnet Lu‐Hf chronology0
Heat sources for Variscan high‐temperature–low‐pressure metamorphism: Petrochronological constraints from the Trois Seigneurs massif, French Pyrenees0
The Diverse Habitats of Eclogite Formation: Insights From the Mesoproterozoic Glenelg Inlier, Scotland0
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Tectonothermal transition from continental collision to post‐collision: Insights from eclogites overprinted in the ultrahigh‐temperature granulite facies (Yadong region, central Himalaya)0
Prograde zircon growth in migmatites0
Exhumation of deep continental crust in a transpressive regime: The example of Variscan eclogites from the Aiguilles‐Rouges massif (Western Alps)0
Unravelling metamorphic ages of suture zone rocks from the Sabzevar and Makran areas (Iran): Robust age constraints for the larger Arabia–Eurasian collision zone0
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The contribution of elastic geothermobarometry to the debate on HP versus UHP metamorphism0
Petrochronology of high‐pressure granulite facies rocks from Southern Brasília Orogen, SE Brazil: Combining quantitative compositional mapping, single‐element thermometry and geochronology0
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The metamorphic footprint of western Laurentia preserved in subducted rocks from southern Australia0
Divergent metamorphism within the Namche Barwa Complex, the Eastern Himalaya, Southeast Tibet, China: Insights from in situ U–Th–Pb dating of metamorphic monazite0
Polyphase Metamorphism of the Northern Rae Craton (Baffin Island, Arctic Canada) and Trace Element Behaviour in Monazite: Insights From Phase Equilibria Modelling and Geochronology0
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Multi‐episodic formation of baddeleyite and zircon in polymetamorphic anorthosite and rutile‐bearing ilmenitite from the Chiapas Massif Complex, Mexico0
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Probing the history of ultra‐high temperature metamorphism through rare earth element diffusion in zircon0
Kinetics and pulses of zircon growth in migmatites beneath a volcanic arc: An example from the high‐T Ryoke Complex, southwest Japan0
Isochemical metamorphism origin of the newly discovered Baqing jadeitoid, eastern‐central Tibet, China0
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, Pakistan0
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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 Syntaxis0
A Cautionary Tale About Not ‘Joining the Dots’ to Infer Anticlockwise P$$ P $$‐T$$ T $$ Paths0
A New UHP‐HP Tectono‐Metamorphic Architecture for the Southern Dora‐Maira Massif Nappe Stack (Western Alps) Based on Petrological and Microstructural Evidence0
Influence of high‐strain deformation on major element mobility in garnet: Nanoscale evidence from atom probe tomography0
Long‐lived high‐grade metamorphism in southern India: Constraints from charnockites and sapphirine‐bearing semipelitic granulites from the Madurai Block0
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