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 2020-11-01 to 2024-11-01.)
ArticleCitations
GeoPS: An interactive visual computing tool for thermodynamic modelling of phase equilibria95
A thermodynamic model for feldspars in KAlSi3O8−NaAlSi3O8−CaAl2Si2O8 for mineral equilibrium calculations24
A window into an older orogenic cycle: P–T conditions and timing of the pre‐Alpine history of the Dora‐Maira Massif (Western Alps)24
The contribution of elastic geothermobarometry to the debate on HP versus UHP metamorphism20
Strengths and limitations of in situ U–Pb titanite petrochronology in polymetamorphic rocks: An example from western Maine, USA19
The pressure–temperature–time–deformation history of the Beni Mzala unit (Upper Sebtides, Rif belt, Morocco): Refining the Alpine tectono‐metamorphic evolution of the Alboran Domain of the western Med17
Anatectic melt inclusions in ultra high temperature granulites17
From microanalysis to supercontinents: Insights from the Rio Apa Terrane into the Mesoproterozoic SW Amazonian Craton evolution during Rodinia assembly17
Thorium zoning in monazite: A case study from the Ivrea–Verbano zone, NW Italy17
Exhumation of deep continental crust in a transpressive regime: The example of Variscan eclogites from the Aiguilles‐Rouges massif (Western Alps)17
Discrimination of thermodynamic and kinetic contributions to the heavy rare earth element patterns in metamorphic garnet16
Late Variscan (315 Ma) subduction or deceptive zircon REE patterns and U–Pb dates from migmatite‐hosted eclogites? (Montagne Noire, France)16
Diachronous collision in the Seve Nappe Complex: Evidence from Lu–Hf geochronology of eclogites (Norrbotten, North Sweden)16
Prograde zircon growth in migmatites16
Carboniferous high‐P metamorphism and deformation in the Belledonne Massif (Western Alps)16
Pressure–temperature–time evolution of subducted crust revealed by complex garnet zoning (Theodul Glacier Unit, Switzerland)15
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 Ocean15
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 dating14
HP tectono‐metamorphic evolution of the Internal Piedmont Zone in Susa Valley (Western Alps): New petrologic insight from garnet+chloritoid‐bearing micaschists and Fe–Ti metagabbro14
Metamorphic evolution and SIMS U–Pb geochronology of orthopyroxene‐bearing high‐Psemipelitic granulite in the Fuping area, middle Trans‐North China Orogen14
Constraining the process of intracontinental subduction in the Austroalpine Nappes: Implications from petrology and Lu‐Hf geochronology of eclogites13
Garnet, zircon, and monazite age and REE signatures in (ultra)high‐temperature and high‐pressure rocks: Examples from the Caledonides and the Pamir13
Self‐induced incipient ‘eclogitization’ of metagranitoids at closed‐system conditions13
Barrovian and Buchan metamorphic series in the Chinese Altai:P–T–t–D evolution and tectonic implications13
Thermal structure in subducted units from continental Moho depths in a palaeo subduction zone, the Asemigawa region of the Sanbagawa metamorphic belt, SW Japan12
Iterative thermodynamic modelling—Part 2: Tracing equilibrium relationships between minerals in metamorphic rocks12
Reconstructing the metamorphic evolution of the Araçuaí orogen (SE Brazil) using in situ U–Pb garnet dating and PT modelling12
Eo‐Variscan metamorphism in the Bohemian Massif: Thermodynamic modelling and monazite geochronology of gneisses and granulites of the Góry Sowie Massif, SW Poland11
Metamorphic evolution of the Great Slave Lake shear zone11
Metamorphic PTtd evolution of the Mesoproterozoic Pur‐Banera supracrustal belt, Aravalli Craton, northwestern India: Insights from phase equilibria modelling and zircon–11
Pronounced and rapid exhumation of the Connecticut Valley Trough revealed through quartz in garnet Raman barometry and diffusion modelling of garnet dissolution–reprecipitation reactions11
Paleoproterozoic ultrahigh‐temperature metamorphism in the Alxa Block, the Khondalite Belt, North China Craton: Petrology and phase equilibria of quartz‐absent corundum‐bearing pelitic granulites11
HTLP metamorphism and fluid‐fluxed melting during multistage anatexis of continental crust (N Sardinia, Italy)10
Delineation of multiple metamorphic events in the Himalayan Kathmandu Complex, central Nepal10
Metapelite from the high‐ to ultrahigh‐pressure terrane of the Eastern Alps (Pohorje Mountains, Slovenia)—New pressure, temperature and time constraints on a polymetamorphic rock10
Tectonothermal transition from continental collision to post‐collision: Insights from eclogites overprinted in the ultrahigh‐temperature granulite facies (Yadong region, central Himalaya)10
Unravelling metamorphic ages of suture zone rocks from the Sabzevar and Makran areas (Iran): Robust age constraints for the larger Arabia–Eurasian collision zone10
What can high‐P sheared orthogneisses tell us? An example from the Curinga–Girifalco Line (Calabria, southern Italy)10
Petrochronology of high‐pressure granulite facies rocks from Southern Brasília Orogen, SE Brazil: Combining quantitative compositional mapping, single‐element thermometry and geochronology9
Partially open grain and phase boundaries as fluid pathways in metamorphic and magmatic rocks9
Drainage of subduction interface fluids into the forearc mantle evidenced by a pristine jadeitite network (Polar Urals)9
Multi‐stage metamorphic history of the Oki gneisses in Japan: Implications for Paleoproterozoic metamorphism and tectonic correlations in northeastern Asia9
A diachronous record of metamorphism in metapelites of the Western Gneiss Region, Norway9
Isothermal compression of an eclogite from the Western Gneiss Region (Norway)9
Garnet as a monitor for melt–rock interaction: Textural, mineralogical, and compositional evidence of partial melting and melt‐driven metasomatism9
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 significance9
Metamorphic transformation rate over large spatial and temporal scales constrained by geophysical data and coupled modelling9
Monazite petrochronology of polymetamorphic granulite‐facies rocks of the Larsemann Hills, Prydz Bay, East Antarctica8
Extensive fluid–rock interaction and pressure solution in a UHP fluid pathway recorded by garnetite, Lago di Cignana, Western Alps8
The controls on the thermal evolution of continental mountain ranges8
Deep subduction, melting, and fast cooling of metapelites from the Cima Lunga Unit, Central Alps8
Th–U powered metamorphism: Thermal consequences of a chemical hotspot8
Peak Alpine metamorphic conditions from staurolite‐bearing metapelites in the Monte Rosa nappe (Central European Alps) and geodynamic implications8
Peritectic minerals record partial melting of the deeply subducted continental crust in the Sulu orogen8
Predicting and explaining crystallographic orientation relationships of exsolved precipitates in garnet using the edge‐to‐edge matching model7
High‐pressure granulite facies re‐equilibration and zoisite–biotite dehydration melting during decompression of an ultrahigh‐pressure garnet clinopyroxenite from the island of Fjørtoft, Norway7
Multi‐mineral petrochronology on a high‐pressure mafic granulite reveals short‐lived high‐temperature metamorphism in the North China Craton7
Tectonic erosion and deep subduction in Central Tibet: Evidence from the discovery of retrograde eclogites in the Amdo microcontinent7
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 Spain7
Constraining the P–T path of (U)HP rocks with reaction overstepping during subduction; example from the Western Gneiss Region (Norway)7
The temporal evolution of subduction initiation in the Samail ophiolite: High‐precision U–Pb zircon petrochronology of the metamorphic sole7
An extensive record of orogenesis recorded in a Madagascar granulite7
Carboniferous–Triassic tectonic and thermal evolution of the middle crust section of the Dervio–Olgiasca Zone (Southern Alps)7
Testing the equilibrium model: An example from the Caledonian Kalak Nappe Complex (Finnmark, Arctic Norway)6
The gabbro to amphibolite transition along a hydration front6
Divergent metamorphism within the Namche Barwa Complex, the Eastern Himalaya, Southeast Tibet, China: Insights from in situ U–Th–Pb dating of metamorphic monazite6
Combined phase diagram modelling and quartz‐in‐garnet barometry of HP metapelites from the Kamieniec Metamorphic Belt (NE Bohemian Massif)6
Ultrahigh‐temperature Palaeoproterozoic rocks in the Neoproterozoic Borborema Province, implications for São Francisco Craton dispersion in NE Brazil6
Kinetics and pulses of zircon growth in migmatites beneath a volcanic arc: An example from the high‐T Ryoke Complex, southwest Japan6
Controls on the scales of equilibrium during granulite facies metamorphism6
Implications of garnet nucleation overstepping for the P–T evolution of the Lesser Himalayan Sequence of central Nepal6
Trace‐element heterogeneity in rutile linked to dislocation structures: Implications for Zr‐in‐rutile geothermometry6
Cryptic evidence for the former presence of lawsonite in blueschist and eclogite6
Phase equilibria and microstructural constraints on the high‐T building of the Kohistan island arc: The Jijal garnet granulites, northern Pakistan6
Petrochronology of polygenetic white micas (Naxos, Greece)6
New constraints on the tectonometamorphic evolution of the Erzgebirge orogenic wedge (Saxothuringian Domain, Bohemian Massif)5
Alpine tectono‐metamorphic evolution of the Corsica basement5
Ultra‐high temperature, mid‐crustal level, contact metamorphism imprinted on granulite facies paragneisses by a norite intrusion (São Gabriel da Baunilha, Araçuaí orogen, southeast Brazil)5
Polymetamorphism during the Grenvillian Orogeny in SE Ontario: Results from trace element mapping, in situ geochronology, and diffusion geospeedometry5
Amalgamation of the Ryoke and Sanbagawa metamorphic belts at the subduction interface: New insights from the Kashio mylonite along the Median Tectonic Line, Nagano, Japan5
Construction of PTt paths for eclogite in the Tongbai orogen by combining phase equilibria modelling with zircon inclusion composition4
Pressure–temperature evolution of the basement and cover sequences on Ios, Greece: Evidence for subduction of the Hercynian basement4
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 Tethysides4
High‐P metamorphism of garnet–epidote–amphibole schists from the Yuli Belt, Eastern Taiwan: Evidence related to warm subduction4
Pressure–temperature–time constraints on gneiss dome formation in an intracontinental orogen4
Pressure–temperature paths of tectonic blocks in mélange: Recording thermal evolution of a subduction channel at an initial stage of subduction4
Redistribution of heat‐producing elements during melting of Archean crust4
H2O in omphacite of quartz and coesite eclogite from Erzgebirge and Fichtelgebirge, Germany4
Metamorphic and chronological constraints on the early Paleozoic tectono‐thermal evolution of the Olkhon Terrane, southern Siberia4
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
Partial melting and reaction along deformation features in plagioclase4
Thermal pulse induced by emplacement of Ramba leucogranites in southern Tibet4
Kyanite preserves prograde and retrograde metamorphic events as revealed by cathodoluminescence, geochemistry, and crystallographic orientation4
The metamorphic PT history of Precambrian Belomorian eclogites (Shirokaya Salma), Russia4
Polyphase tectonic reworking of serpentinites and chlorite‐tremolite‐talc rocks (SW Spain) from the subduction forearc to intracontinental emplacement4
Probing the history of ultra‐high temperature metamorphism through rare earth element diffusion in zircon3
Lu–Hf garnet dating and the timing of collisions: Palaeoproterozoic accretionary tectonics revealed in the Southeastern Churchill Province, Trans‐Hudson Orogen, Canada3
Preservation of mantle heterogeneities and serpentinization signature during antigorite dehydration: The example of the Bergell contact aureole3
P–T–t–D records of Early Palaeozoic Andean‐type shortening of a hot active margin: The Dunhuang block in NW China3
To be or not to be Alpine: New petrological constraints on the metamorphism of the Chenaillet Ophiolite (Western Alps)3
40Ar/39Ar dates controlled by white mica deformation and strain localization: Insights from comparing in situ laser ablation and single‐grain fusion techniques3
Petrochronologic constraints on inverted metamorphism, terrane accretion, thrust stacking, and ductile flow in the Gneiss Dome belt, northern Appalachian orogen3
Regional high‐T/low‐P metamorphism of the Kemum Basement High, Bird’s Head, West Papua, Indonesia3
Alpine subduction zone metamorphism in the Palaeozoic successions of the Monti Romani (Northern Apennines, Italy)3
Garnet crystallization mechanisms and localized polymetamorphism in the southwestern Meguma Terrane, Nova Scotia, Canada3
Paleoarchean metamorphism in the Acasta Gneiss Complex: Constraints from phase equilibrium modelling and in situ garnet Lu–Hf geochronology3
Low temperature eclogite facies rocks discovered in the Eastern Himalayan Syntaxis: Poly‐cyclic metamorphic evolution and implications3
Low‐grade prehnite‐pumpellyite facies metamorphism and metasomatism in basement rocks adjacent to the Permian Oslo rift: The importance of displacive reactions3
Multi‐episodic formation of baddeleyite and zircon in polymetamorphic anorthosite and rutile‐bearing ilmenitite from the Chiapas Massif Complex, Mexico2
Ultrahigh thermal gradient granulites in the Narryer Terrane, Yilgarn Craton, Western Australia, provide a window into the composition and formation of Archean lower crust2
Formation of multistage garnet grains by fragmentation and overgrowth constrained by microchemical and microstructural mapping2
Disruption of a high‐pressure unit during exhumation: Example of the Cycladic Blueschist unit (Thera, Ios and Naxos islands, Greece)2
Garnet growth and mineral geochronology constrains the diachronous Neoproterozoic convergent evolution of the southern Dom Feliciano Belt, Uruguay2
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 Alps2
Chromium in minerals as tracer of the polycyclic evolution of eclogite and related metabasite from the Pohorje Mountains, Slovenian Eastern Alps2
Trapped K‐feldspar phenocrysts as a signature of melt migration pathways within active high‐strain zones2
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 Caledonides2
Protracted eclogite‐facies metamorphism of the Dulan area, North Qaidam ultrahigh‐pressure terrane: Insights on zircon growth during continental subduction and collision2
Gabbroic eclogites formed during rapid and cold subduction of the Paleo‐Tethys oceanic lithosphere in the Changning–Menglian orogenic belt, southeastern Tibetan plateau2
Assessing the importance of H2O content in the tectono‐metamorphic evolution of shear zones: A case study from the Dora‐Maira Massif (Western Alps)2
Pattern and source of unusually high‐temperature metamorphism in an Eocene forearc recorded by the Pacific Rim Terrane, British Columbia, Canada2
Retentiveness of rare earth elements in garnet with implications for garnet Lu‐Hf chronology2
Effects of Fe3+ in sillimanite on mineral stabilities and parageneses in ultrahigh‐temperature metapelites2
Deviation between quartz‐in‐garnet elastic geobarometry and equilibrium‐based pressure–temperature modelling in Barrovian metamorphic rocks2
Bulk inclusion micro‐zircon U–Pb geochronology: A new tool to date low‐grade metamorphism2
The slab–mantle wedge interface of an incipient subduction zone: Insights from the PTD evolution and petrological characteristics of the Dalrymple Amphibolite, Palawan Ophiolite2
The origin and compositions of melt inclusions in an Al2SiO5‐free paragneiss from the Namche Barwa Complex in the Eastern Himalayan Syntaxis1
Complex geochronological record of an emblematic Variscan eclogite (Haut‐Allier, French Massif Central)1
A rutile and titanite record of subduction fluids: Integrated oxygen isotope and trace element analyses in Franciscan high‐pressure rocks1
Mechanisms and durations of metamorphic garnet crystallization in the lower nappes of the Caledonian Kalak Nappe Complex, Arctic Norway1
Influence of high‐strain deformation on major element mobility in garnet: Nanoscale evidence from atom probe tomography1
An Iapetus origin for a layered eclogite complex in the northern Western Gneiss Region, Scandinavian Caledonides1
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 ma1
Constraints on the Palaeoproterozoic tectono‐metamorphic evolution of the Lewisian Gneiss Complex, NW Scotland: Implications for Nuna assembly1
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
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)1
Deformation‐induced graphitization and muscovite recrystallization in a ductile fault zone1
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
The inhibited response of accessory minerals during high‐temperature reworking1
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