Journal of Metamorphic Geology

Papers
(The TQCC of Journal of Metamorphic Geology is 5. 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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A Prograde Dual‐Segmented Geotherm for (Retro‐) Eclogite From Western Dabie and Implications for Maximum Decoupling Depths During Continental Subduction20
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Significance of selective crystal entrainment and differential crystal‐melt separation in petrogenesis of granites from the Tongbai orogen20
Bulk inclusion micro‐zircon U–Pb geochronology: A new tool to date low‐grade metamorphism19
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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
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Multi‐mineral petrochronology on a high‐pressure mafic granulite reveals short‐lived high‐temperature metamorphism in the North China Craton17
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The inhibited response of accessory minerals during high‐temperature reworking15
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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
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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
Editorial14
Low‐grade prehnite‐pumpellyite facies metamorphism and metasomatism in basement rocks adjacent to the Permian Oslo rift: The importance of displacive reactions14
Partial melting mechanisms of peraluminous felsic magmatism in a collisional orogen: An example from the Khondalite belt, North China craton13
Alpine subduction zone metamorphism in the Palaeozoic successions of the Monti Romani (Northern Apennines, Italy)13
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
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
Zircon Coupled Dissolution–Precipitation Replacement During Melt–Rock Interaction Modifies Chemical Signatures Resulting in Misleading Ages11
Thorium zoning in monazite: A case study from the Ivrea–Verbano zone, NW Italy10
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
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
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
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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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
The tempo and conditions of metamorphism during magmatism, southern Coast Mountains batholith, British Columbia, Canada7
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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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
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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Metasomatism of the continental crust and its impact on surface uplift: Insights from reactive‐transport modelling5
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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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