All Stories

  1. Garnet as a reliable timekeeper in Archean polymetamorphic terranes
  2. The evolution of Earth’s early continental crust
  3. An exogenic to endogenic thermal transition on Earth 3.9 billion years ago
  4. Incipient continent formation by shallow melting of an altered mafic protocrust
  5. A potential mantle origin for precursor rocks of high-Mg impact glass beads in Chang’e-5 soil
  6. Formation and composition of Earth’s Hadean protocrust
  7. Subducted magnesite in serpentinite carries fluid-mobile elements and carbon into the lower mantle
  8. A Paleoarchaean impact crater in the Pilbara Craton, Western Australia
  9. Enhanced subduction flux during the assembly of Pangea recorded by global intracontinental magmatism
  10. Fresh water on Earth four billion years ago
  11. Global mantle perturbations following the onset of modern plate tectonics
  12. Is plate tectonics a post-Archean phenomenon? A petrological perspective
  13. Onset of the Earth’s hydrological cycle four billion years ago or earlier
  14. Paleoarchean metamorphism in the Acasta Gneiss Complex: Constraints from phase equilibrium modelling and in situ garnet Lu–Hf geochronology
  15. Bimodality in zircon oxygen isotopes and implications for crustal melting on the early Earth
  16. Changes in orogenic style and surface environment recorded in Paleoproterozoic foreland successions
  17. Giant impacts and the origin and evolution of continents
  18. Multiple dates in millimetres; diffusion as an explanation for Rb-Sr age discrepancies in biotite
  19. Pressure–temperature conditions and age of metamorphism in the Archean Acasta Gneiss Complex: constraints from phase equilibrium modelling and in situ garnet Lu-Hf geochronology
  20. Ultra-slow cooling of ultra-hot orogens
  21. Greenstone burial–exhumation cycles at the late Archean transition to plate tectonics
  22. Coexisting divergent and convergent plate boundary assemblages indicate plate tectonics in the Neoarchean
  23. Giant impacts and the origin and evolution of continents
  24. Secular changes in metamorphism and metamorphic cooling rates track the evolving plate-tectonic regime on Earth
  25. Experimental constraints on the long-lived radiogenic isotope evolution of the Moon
  26. Newly-discovered ultra-high temperature granulites from the East Hebei terrane, North China Craton
  27. How old are the Jack Hills metasediments really?: The case for contamination of bedrock by zircon grains in transported regolith
  28. Linking metamorphism and plate boundaries over the past 2 billion years
  29. Geology Bites podcast by Oliver Strimpel
  30. Closing the “North American Magmatic” Gap: Crustal evolution of the Clearwater Block from multi-isotope and trace element zircon data
  31. Pb isotope insight into the formation of the Earth's first stable continents
  32. Boninitic blueschists record subduction initiation and subsequent accretion of an arc–forearc in the northeast Proto-Tethys Ocean
  33. Detrital zircon U–Pb and Hf signatures of Paleo-Mesoproterozoic strata in the Priest River region, northwestern USA: A record of Laurentia assembly and Nuna tenure
  34. Model versus measured detrital zircon age signatures of the early Earth
  35. Metasediment-derived Melts in Subduction-zone Magmas and their Influence on Crustal Evolution
  36. A model for evolving crust on 4 Vesta through combined compositional and thermal modelling
  37. Crustal melting and suprasolidus phase equilibria: From first principles to the state-of-the-art
  38. Recovering P–T–t paths from ultra-high temperature (UHT) felsic orthogneiss: An example from the Southern Brasília Orogen, Brazil
  39. Continental basalts track secular cooling of the mantle and the onset of modern plate tectonics
  40. Using zircon in mafic migmatites to disentangle complex high-grade gneiss terrains – Terrane spotting in the Lewisian complex, NW Scotland
  41. Formation and Evolution of a Neoproterozoic Continental Magmatic Arc
  42. Oxygen isotopes trace the origins of Earth’s earliest continental crust
  43. Geology of non-plate tectonic regimes: detrital zircon age records and beyond
  44. Partial Melting of Bimineralic Eclogite by Clinopyroxene Breakdown 
  45. Zircon U-Pb and Lu-Hf record from the Archean Lewisian Gneiss Complex, NW Scotland
  46. Recalibrating Rodinian rifting in the northwestern United States
  47. The phases of the Moon: Modelling crystallisation of the lunar magma ocean through equilibrium thermodynamics
  48. Controls on the scales of equilibrium during granulite facies metamorphism
  49. Partial melting of ultrahigh-pressure eclogite by omphacite-breakdown facilitates exhumation of deeply-subducted crust
  50. Theoretical versus empirical secular change in zircon composition
  51. The internal structure and geodynamics of Mars inferred from a 4.2-Gyr zircon record
  52. TTG generation by fluid-fluxed crustal melting: Direct evidence from the Proterozoic Georgetown Inlier, NE Australia
  53. Paired metamorphism in the Neoarchean: A record of accretionary-to-collisional orogenesis in the North China Craton
  54. A Baltic heritage in Scotland: Basement terrane transfer during the Grenvillian orogeny
  55. Plate Tectonics and the Archean Earth
  56. Critical role of water in the formation of continental crust
  57. Petrogenesis of leucosome sheets in migmatitic UHP eclogites—Evolution from silicate-rich supercritical fluid to hydrous melt
  58. A review of the chondrite–achondrite transition, and a metamorphic facies series for equilibrated primitive stony meteorites
  59. Persistence of melt-bearing Archean lower crust for >200 m.y.— An example from the Lewisian Complex, northwest Scotland
  60. Quantitative automated mineralogy to constrain metamorphic processes using ZEISS Mineralogic
  61. Evolution of geodynamics since the Archean: Significant change at the dawn of the Phanerozoic
  62. Modelling U-Pb discordance in the Acasta Gneiss: Implications for fluid–rock interaction in Earth's oldest dated crust
  63. Persistence of melt-bearing Archean lower crust for >200 m.y.—An example from the Lewisian Complex, northwest Scotland
  64. No evidence for high-pressure melting of Earth’s crust in the Archean
  65. Garnet, the archetypal cubic mineral, grows tetragonal
  66. The Mangaroon Orogeny: Synchronous c. 1.7 Ga magmatism and low-P, high-T metamorphism in the West Australian Craton
  67. Into the melting pot: A celebration of the career of Michael Brown
  68. Metamorphism and the evolution of subduction on Earth
  69. Metamorphism and the evolution of plate tectonics
  70. Testing the fidelity of thermometers at ultrahigh temperatures
  71. Time's arrow, time's cycle: Granulite metamorphism and geodynamics
  72. Closed system behaviour of argon in osumilite records protracted high‐ T metamorphism within the Rogaland–Vest Agder Sector, Norway
  73. Corrigendum to: ’Modelling the Hafnium–Neodymium Evolution of Early Earth: A Study from West Greenland’
  74. Antimony in rutile as a pathfinder for orogenic gold deposits
  75. Nanoscale constraints on the shock-induced transformation of zircon to reidite
  76. Performing process-oriented investigations involving mass transfer using Rcrust: a new phase equilibrium modelling tool
  77. Zircon U–Pb, Lu–Hf and O isotopes from the 3414 Ma Strelley Pool Formation, East Pilbara Terrane, and the Palaeoarchaean emergence of a cryptic cratonic core
  78. Secular change in TTG compositions: Implications for the evolution of Archaean geodynamics
  79. A window into an ancient backarc? The magmatic and metamorphic history of the Fraser Zone, Western Australia
  80. Modelling the Hafnium–Neodymium Evolution of Early Earth: A Study from West Greenland
  81. Neoproterozoic evolution and Cambrian reworking of ultrahigh temperature granulites in the Eastern Ghats Province, India
  82. Zircon as a metamorphic timekeeper: A case study from the Caledonides of central Norway
  83. An impact melt origin for Earth’s oldest known evolved rocks
  84. New constraints on granulite facies metamorphism and melt production in the Lewisian Complex, northwest Scotland
  85. Secular change in metamorphism and the onset of global plate tectonics
  86. Melting controls on the lutetium–hafnium evolution of Archaean crust
  87. Zircon geochronology reveals polyphase magmatism and crustal anatexis in the Buchan Block, NE Scotland: Implications for the Grampian Orogeny
  88. Processes of crust formation in the early Earth imaged through Hf isotopes from the East Pilbara Terrane
  89. Fluid generation and evolution during exhumation of deeply subducted UHP continental crust: Petrogenesis of composite granite-quartz veins in the Sulu belt, China
  90. Earth’s first stable continents did not form by subduction
  91. Reappraising the P–T evolution of the Rogaland–Vest Agder Sector, southwestern Norway
  92. Mechanisms of deformation-induced trace element migration in zircon resolved by atom probe and correlative microscopy
  93. se-2016-97. Arrested development – a comparative analysis of multilayer corona textures in metamorphic rocks
  94. Subduction or sagduction? Ambiguity in constraining the origin of ultramafic–mafic bodies in the Archean crust of NW Scotland
  95. Grain size matters: Implications for element and isotopic mobility in titanite
  96. Constraints on the timing and conditions of high-grade metamorphism, charnockite formation and fluid-rock interaction in the Trivandrum Block, southern India
  97. The source of Dalradian detritus in the Buchan Block, NE Scotland: application of new tools to detrital datasets
  98. Discriminating prolonged, episodic or disturbed monazite age spectra: An example from the Kalak Nappe Complex, Arctic Norway
  99. Metamorphism and partial melting of ordinary chondrites: Calculated phase equilibria
  100. Hot orogens and supercontinent amalgamation: A Gondwanan example from southern India
  101. Precambrian reidite discovered in shocked zircon from the Stac Fada impactite, Scotland
  102. Grampian migmatites in the Buchan Block
  103. Unravelling the complexities in high-grade rocks using multiple techniques: the Achankovil Zone of southern India
  104. Prograde and retrograde growth of monazite in migmatites: An example from the Nagercoil Block, southern India
  105. The effect of Mn on mineral stability in metapelites revisited: newa-xrelations for manganese-bearing minerals
  106. Partial melting of metabasic rocks in Val Strona di Omegna, Ivrea Zone, northern Italy
  107. New mineral activity-composition relations for thermodynamic calculations in metapelitic systems
  108. Thermobarometric constraints on pressure variations across the Plattengneiss shear zone of the Eastern Alps: implications for exhumation models during Eoalpine subduction
  109. Delamination and recycling of Archaean crust caused by gravitational instabilities
  110. Migmatites in the Ivrea Zone (NW Italy): Constraints on partial melting and melt loss in metasedimentary rocks from Val Strona di Omegna
  111. Field and petrographic evidence for partial melting of TTG gneisses from the central region of the mainland Lewisian complex, NW Scotland
  112. Polymetamorphism in the mainland Lewisian complex, NW Scotland - phase equilibria and geochronological constraints from the Cnoc an t’Sidhean suite
  113. Archaean Intracrustal Differentiation from Partial Melting of Metagabbro--Field and Geochemical Evidence from the Central Region of the Lewisian Complex, NW Scotland
  114. Phase equilibrium constraints on a deep crustal metamorphic field gradient: metapelitic rocks from the Ivrea Zone (NW Italy)
  115. Is the Crucible Reproducible? Reconciling Melting Experiments with Thermodynamic Calculations
  116. A year in the life of an aluminous metapelite xenolith—The role of heating rates, reaction overstep, H2O retention and melt loss
  117. Phase equilibrium constraints on conditions of granulite-facies metamorphism at Scourie, NW Scotland
  118. Petrogenetic modelling of strongly residual metapelitic xenoliths within the southern Platreef, Bushveld Complex, South Africa
  119. Partial melting of metagreywacke: a calculated mineral equilibria study
  120. Spinel-cordierite symplectites replacing andalusite: evidence for melt-assisted diapirism in the Bushveld Complex, South Africa
  121. Constraints on the tectonometamorphic evolution of the Western Ethiopian Shield
  122. Quantitative Constraints on Metamorphism in the Variscides of Southern Brittany--a Complementary Pseudosection Approach
  123. Evidence for a genetic granite–migmatite link in the Dalradian of NE Scotland
  124. Melt segregation structures within the Inzie Head gneisses of the northeastern Dalradian
  125. Partial melting in the Inzie Head gneisses: the role of water and a petrogenetic grid in KFMASH applicable to anatectic pelitic migmatites
  126. Wollastonite-bearing assemblages from the Dalradian at Fraserburgh, northeast Scotland and their bearing on the emplacement of garnetiferous granitoid sheets