Journal of Metamorphic Geology

Papers
(The H4-Index of Journal of Metamorphic Geology is 15. 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 2021-05-01 to 2025-05-01.)
ArticleCitations
Issue Information136
Significance of selective crystal entrainment and differential crystal‐melt separation in petrogenesis of granites from the Tongbai orogen45
Low‐grade prehnite‐pumpellyite facies metamorphism and metasomatism in basement rocks adjacent to the Permian Oslo rift: The importance of displacive reactions29
A buried gneiss dome in the northern Gawler Craton: The record of early Mesoproterozoic (ca. 1600–1560 Ma) extension in southern Proterozoic Australia25
22
Constraining the P–T path of (U)HP rocks with reaction overstepping during subduction; example from the Western Gneiss Region (Norway)22
Hydration of mafic crustal rocks at high temperature during brittle‐viscous deformation along a strike‐slip plate boundary22
Pressure–temperature paths of tectonic blocks in mélange: Recording thermal evolution of a subduction channel at an initial stage of subduction22
Petrochronology of polygenetic white micas (Naxos, Greece)21
Thermal pulse induced by emplacement of Ramba leucogranites in southern Tibet20
Issue Information20
A thermodynamic model for feldspars in KAlSi3O8−NaAlSi3O8−CaAl2Si2O8 for mineral equilibrium calculations20
Polyphase tectonic reworking of serpentinites and chlorite‐tremolite‐talc rocks (SW Spain) from the subduction forearc to intracontinental emplacement19
Cover Image17
Thermodynamic constraints on the composition of orogenically thickened lower crust16
15
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 Asia15
The Structure and P–T–t–d Evolution of the Saxothuringian/Brunovistulian Variscan Boundary Zone in the Bohemian Massif (Czech Republic, Poland)15
Carboniferous Barrovian to Permian Buchan‐type metamorphic cycles in the Mongolian Altai Zone: Implication for pressure cycles in accretionary orogens15
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