This work is licensed under the Creative Commons Attribution 4.0 International License.
Ague, J.J. (1994). Mass transfer during barrovian meta-morphism of pelites. American Journal of Science, 294, 986-1057.AgueJ.J.(1994).Mass transfer during barrovian meta-morphism of pelites.,294,986-1057.Search in Google Scholar
Ague, J.J. (2003). Fluid infiltration and transport of major, minor, and trace elements during regional metamorphism of carbonate rocks, Wepawaug Schist, Connecticut, USA. American Journal of Science, 303(9), 753-816.AgueJ.J.(2003).Fluid infiltration and transport of major, minor, and trace elements during regional metamorphism of carbonate rocks, Wepawaug Schist, Connecticut, USA.,303(9),753-816.Search in Google Scholar
Ague, J.J. (2011). Extreme channelization of fluid and the problem of element mobility during Barrovian metamorphism. American Mineralogist, 96(2-3), 333-352.AgueJ.J.(2011).Extreme channelization of fluid and the problem of element mobility during Barrovian metamorphism.,96(2-3),333-352.Search in Google Scholar
Ague, J.J., & Van Haren, J.L.M. (1996). Assessing metasomatic mass and volume changes using the bootstrap, with application to deep crustal hydrothermal alteration of marble. Economic Geology, 91(7), 1169-1182.AgueJ.J., &Van HarenJ.L.M.(1996).Assessing metasomatic mass and volume changes using the bootstrap, with application to deep crustal hydrothermal alteration of marble.,91(7),1169-1182.Search in Google Scholar
Alderton, D.H.M., Pearce, J.A. & Potts, PJ. (1980). Rare earth element mobility during granite alteration: evidence from southwest England. Earth and Planetary Science Letters, 49(1), 149-165.AldertonD.H.M.PearceJ.A., &PottsPJ.(1980).Rare earth element mobility during granite alteration: evidence from southwest England.,49(1),149-165.Search in Google Scholar
Baños, J.O., & Amouric, M. (1984). Biotite chloritization by interlayer brucitization as seen by HRTEM. American Mineralogist, 69(9–10), 869–871.BañosJ.O., &AmouricM.(1984).Biotite chloritization by interlayer brucitization as seen by HRTEM.,69(9–10),869–871.Search in Google Scholar
Baumgartner, L.P., & Olsen, S.N. (1995). A least-squares approach to mass transport calculations using the isocon method. Economic Geology, 90(5), 1261–1270.BaumgartnerL.P., &OlsenS.N.(1995).A least-squares approach to mass transport calculations using the isocon method.,90(5),1261–1270.Search in Google Scholar
Bucher, K., & Grapes, R. (2011). Petrogenesis of metamorphic rocks. Springer Berlin, Heidelberg.BucherK., &GrapesR.(2011)..Springer Berlin,Heidelberg.Search in Google Scholar
Centrella, S., Austrheim, H., & Putnis, A. (2015). Coupled mass transfer through a fluid phase and volume preservation during the hydration of granulite: An example from the Bergen Arcs, Norway. Lithos, 236–237, 245–255.CentrellaS.AustrheimH., &PutnisA.(2015).Coupled mass transfer through a fluid phase and volume preservation during the hydration of granulite: An example from the Bergen Arcs, Norway.,236–237,245–255.Search in Google Scholar
Centrella, S., Putnis, A., Lanari, P., & Austrheim, H. (2018). Textural and chemical evolution of pyroxene during hydration and deformation: a consequence of retrograde metamorphism. Lithos, 296, 245-264.CentrellaS.PutnisA.LanariP., &AustrheimH.(2018).Textural and chemical evolution of pyroxene during hydration and deformation: a consequence of retrograde metamorphism.,296,245-264.Search in Google Scholar
Centrella, S., Beaudoin, N.E., Derluyn, H., Motte, G., Hoareau, G., Lanari, P., Piccoli, F., Pécheyran, C. and Callot, J.P. (2021). Micro-scale chemical and physical patterns in an interface of hydrothermal dolomitization reveals the governing transport mechanisms in nature: Case of the Layens anticline, Pyrenees, France. Sedimentology, 68(2), 834–854.CentrellaS.BeaudoinN.E.DerluynH.MotteG.HoareauG.LanariP.PiccoliF.PécheyranC.CallotJ.P.(2021).Micro-scale chemical and physical patterns in an interface of hydrothermal dolomitization reveals the governing transport mechanisms in nature: Case of the Layens anticline, Pyrenees, France.,68(2),834–854.Search in Google Scholar
Condie, K.C., & Sinha, A.K. (1996). Rare earth and other trace element mobility during mylonitization: a comparison of the Brevard and Hope Valley shear zones in the Appalachian Mountains, USA. Journal of Metamorphic Geology, 14(2), 213–226.CondieK.C., &SinhaA.K.(1996).Rare earth and other trace element mobility during mylonitization: a comparison of the Brevard and Hope Valley shear zones in the Appalachian Mountains, USA.,14(2),213–226.Search in Google Scholar
Dallmann, W.K., & Piepjohn, K. (2020). The structure of the Old Red Sandstone and the Svalbardian Orogenic Event (Ellesmerian Orogeny) in Svalbard. Norg. Geol. Unders. B, 15, 1–106.DallmannW.K., &PiepjohnK.(2020).The structure of the Old Red Sandstone and the Svalbardian Orogenic Event (Ellesmerian Orogeny) in Svalbard.,15,1–106.Search in Google Scholar
Durand, C., Oliot, E., Marquer, D., & Sizun, J.P. (2015). Chemical mass transfer in shear zones and metacarbonate xenoliths: a comparison of four mass balance approaches. European Journal of Mineralogy, 27(6), 731–754.DurandC.OliotE.MarquerD., &SizunJ.P.(2015).Chemical mass transfer in shear zones and metacarbonate xenoliths: a comparison of four mass balance approaches.27(6),731–754.Search in Google Scholar
Eggleton, R.A., & Banfield, J.F. (1985). The alteration of granitic biotite to chlorite. American Mineralogist, 70(9–10), 902–910.EggletonR.A., &BanfieldJ.F.(1985).The alteration of granitic biotite to chlorite.,70(9–10),902–910.Search in Google Scholar
Faehnrich, K., Majka, J., Schneider, D., Mazur, S., Manecki, M., Ziemniak, G., Wala, V.T. & Strauss, J.V. (2020). Geochronological constraints on Caledonian strike– slip displacement in Svalbard, with implications for the evolution of the Arctic. Terra Nova, 32(4), 290-299.FaehnrichK.MajkaJ.SchneiderD.MazurS.ManeckiM.ZiemniakG.WalaV.T., &StraussJ.V.(2020).Geochronological constraints on Caledonian strike– slip displacement in Svalbard, with implications for the evolution of the Arctic.,32(4),290-299.Search in Google Scholar
Ferry, J.M. (1979). Reaction mechanisms, physical conditions, and mass transfer during hydrothermal alteration of mica and feldspar in granitic rocks from south central Maine, USA. Contributions to Mineralogy and Petrology, 68(2), 125–139.FerryJ.M.(1979).Reaction mechanisms, physical conditions, and mass transfer during hydrothermal alteration of mica and feldspar in granitic rocks from south central Maine, USA.,68(2),125–139.Search in Google Scholar
Freiberger, R., Hecht, L., Cuney, M., & Morteani, G. (2001). Secondary Ca–Al silicates in plutonic rocks: implications for their cooling history. Contributions to Mineralogy and Petrology, 141(4), 415-429.FreibergerR.HechtL.CuneyM., &MorteaniG.(2001).Secondary Ca–Al silicates in plutonic rocks: implications for their cooling history.,141(4),415-429.Search in Google Scholar
Gee, D.G., & Teben’kov, A.M. (2004). Svalbard: a fragment of the Laurentian margin. Geological Society, London, Memoirs, 30(1), 191-206.GeeD.G., &Teben’kovA.M.(2004).Svalbard: a fragment of the Laurentian margin.,30(1),191-206.Search in Google Scholar
Goncalves, P., Marquer, D., Oliot, E., & Durand, C. (2013). Thermodynamic modeling and thermobarometry of metasomatized rocks. In D.E. Harlov & H. Austrheim (Eds.), Metasomatism and the Chemical Transformation of Rock (pp. 53-91). Springer, Berlin, Heidelberg.GoncalvesP.MarquerD.OliotE., &DurandC.(2013).Thermodynamic modeling and thermobarometry of metasomatized rocks.InHarlovD.E., &AustrheimH.(Eds.),(pp.53-91).Springer, Berlin,Heidelberg.Search in Google Scholar
Grant, J.A. (1986). The isocon diagram; a simple solution to Gresens’ equation for metasomatic alteration. Economic Geology, 81(8), 1976–1982.GrantJ.A.(1986).The isocon diagram; a simple solution to Gresens’ equation for metasomatic alteration.,81(8),1976–1982.Search in Google Scholar
Grant, J.A. (2005). Isocon analysis: A brief review of the method and applications. Physics and Chemistry of the Earth, 30(17–18), 997–1004.GrantJ.A.(2005).Isocon analysis: A brief review of the method and applications.,30(17–18),997–1004.Search in Google Scholar
Gresens, R.L. (1967). Composition-volume relationships of metasomatism. Chemical Geology, 2, 47-65.GresensR.L.(1967).Composition-volume relationships of metasomatism.,2,47-65.Search in Google Scholar
Harland, W. B., Scott, R. A., Aukland, K. A., & Snape, I. (1992). The Ny Friesland Orogen, Spitsbergen. Geological Magazine, 129, 679-708.HarlandW. B.ScottR. A.AuklandK. A., &SnapeI.(1992).The Ny Friesland Orogen, Spitsbergen.,129,679-708.Search in Google Scholar
Harland, W.B., Cutbill, J.L., Friend, P.F., Gobbett, D.J., Holliday, D.W., Maton, P.I., Parker, J.R. & Wallis, R.H. (1974). The Billefjorden Fault Zone, Spitsbergen: the long history of a major tectonic lineament. Norsk Polarinstitutt Tiddskrifter, 161, 1-72.HarlandW.B.CutbillJ.L.FriendP.F.GobbettD.J.HollidayD.W.MatonP.I.ParkerJ.R., &WallisR.H.(1974).The Billefjorden Fault Zone, Spitsbergen: the long history of a major tectonic lineament.,161,1-72.Search in Google Scholar
Harlov, D.E., Wirth, R., & Hetherington, C.J. (2011). Fluid-mediated partial alteration in monazite: the role of coupled dissolution-reprecipitation in element redistribution and mass transfer. Contributions to Mineralogy and Petrology, 162(2), 329-348.HarlovD.E.WirthR., &HetheringtonC.J.(2011).Fluid-mediated partial alteration in monazite: the role of coupled dissolution-reprecipitation in element redistribution and mass transfer.,162(2),329-348.Search in Google Scholar
Hey, M.H. (1954). A New Review of the Chlorites. Mineralogical Magazine, 30(224), 277-292.HeyM.H.(1954).A New Review of the Chlorites.,30(224),277-292.Search in Google Scholar
Janoušek, V., Farrow, C.M., & Erban, V. (2006). Interpretation of whole-rock geochemical data in igneous geochemistry: Introducing Geochemical Data Toolkit (GCDkit). Journal of Petrology, 47(6), 1255-1259.JanoušekV.FarrowC.M., &ErbanV.(2006).Interpretation of whole-rock geochemical data in igneous geochemistry: Introducing Geochemical Data Toolkit (GCDkit).,47(6),1255-1259.Search in Google Scholar
Kelemen, P.B., & Matter, J. (2008). In situ carbonation of peridotite for CO2 storage. Proceedings of the National Academy of Sciences, 105(45), 17295-17300.KelemenP.B., &MatterJ.(2008).In situ carbonation of peridotite for CO2 storage.,105(45),17295-17300.Search in Google Scholar
Kogure, T., & Banfield, J.F. (2000). New insights into the mechanism for chloritization of biotite using polytype analysis. American Mineralogist, 85(9), 1202-1208.KogureT., &BanfieldJ.F.(2000).New insights into the mechanism for chloritization of biotite using polytype analysis.,85(9),1202-1208.Search in Google Scholar
Lanari, P., Vho, A., Bovay, T., Airaghi, L. & Centrella, S. (2019). Quantitative compositional mapping of mineral phases by electron probe micro-analyser. Geological Society, London, Special Publications, 478(1), 39-63.LanariP.VhoA.BovayT.AiraghiL., &CentrellaS.(2019).Quantitative compositional mapping of mineral phases by electron probe micro-analyser.,478(1),39-63.Search in Google Scholar
Lanari, P., Vidal, O., De Andrade, V., Dubacq, B., Lewin, E., Grosch, E. G. & Schwartz, S., (2014). XMapTools: A MATLAB-based program for electron microprobe X-ray image processing and geothermobarometry. Computers and Geosciences, 62, 227-240.LanariP.VidalO.De AndradeV.DubacqB.LewinE.GroschE. G., &SchwartzS., (2014).XMapTools: A MATLAB-based program for electron microprobe X-ray image processing and geothermobarometry.,62,227-240.Search in Google Scholar
Majka, J., & Kośmińska, K. (2017). Magmatic and metamorphic events recorded within the Southwestern Basement Province of Svalbard. arktos, 3(1), 1-7.MajkaJ., &KośmińskaK.(2017).Magmatic and metamorphic events recorded within the Southwestern Basement Province of Svalbard.,3(1),1-7.Search in Google Scholar
Merino, E. & Canals, À. (2011). Self-accelerating dolomite-for-calcite replacement: Self-organized dynamics of burial dolomitization and associated mineralization. American Journal of Science, 311(7), 573-607.MerinoE., &CanalsÀ.(2011).Self-accelerating dolomite-for-calcite replacement: Self-organized dynamics of burial dolomitization and associated mineralization.,311(7),573-607.Search in Google Scholar
McCann, A.J., & Dallmann, W.K. (1996). Reactivation history of the long-lived Billefjorden Fault Zone in north central Spitsbergen, Svalbard. Geological Magazine, 133(1), 63-84.McCannA.J., &DallmannW.K.(1996).Reactivation history of the long-lived Billefjorden Fault Zone in north central Spitsbergen, Svalbard.,133(1),63-84.Search in Google Scholar
Moore, J., Beinlich, A., Austrheim, H., & Putnis, A. (2019). Stress orientation-dependent reactions during metamorphism. Geology, 47(2), 151-154.MooreJ.BeinlichA.AustrheimH., &PutnisA.(2019).Stress orientation-dependent reactions during metamorphism.,47(2),151-154.Search in Google Scholar
Olsen, S.N. & Grant, J.A. (1991). Isocon analysis of migmatization in the Front Range, Colorado, USA. Journal of Metamorphic Geology, 9(2), 151–164.OlsenS.N., &GrantJ.A.(1991).Isocon analysis of migmatization in the Front Range, Colorado, USA.,9(2),151–164.Search in Google Scholar
Osterberg, S.A., Morton, R.L., & Franklin, J.M. (1987). Hydrothermal alteration and physical volcanology of Archean rocks in the vicinity of the Headway Coulee massive sulfide occurrence, Onaman area, northwestern Ontario. Economic Geology, 82(6), 1505–1520.OsterbergS.A.MortonR.L., &FranklinJ.M.(1987).Hydrothermal alteration and physical volcanology of Archean rocks in the vicinity of the Headway Coulee massive sulfide occurrence, Onaman area, northwestern Ontario.,82(6),1505–1520.Search in Google Scholar
Parneix, J.C., Beaufort, D., Dudoignon, P., & Meunier, A. (1985). Biotite chloritization process in hydrothermally altered granites. Chemical Geology, 51(1-2), 89–101.ParneixJ.C.BeaufortD.DudoignonP., &MeunierA.(1985).Biotite chloritization process in hydrothermally altered granites.,51(1-2),89–101.Search in Google Scholar
Parry, W.T., & Downey, L.M. (1982). Geochemistry of Hydrothermal Chlorite Replacing Igneous Biotite. Clays and Clay Minerals, 30(2), 81–90.ParryW.T., &DowneyL.M.(1982).Geochemistry of Hydrothermal Chlorite Replacing Igneous Biotite.,30(2),81–90.Search in Google Scholar
Plümper, O., & Putnis, A. (2009). The complex hydrothermal history of granitic rocks: multiple feldspar replacement reactions under subsolidus conditions. Journal of Petrology, 50(5), 967–987.PlümperO., &PutnisA.(2009).The complex hydrothermal history of granitic rocks: multiple feldspar replacement reactions under subsolidus conditions.,50(5),967–987.Search in Google Scholar
Potdevin, J.L., & Marquer, D. (1987). Quantitative Methods for the Estimation of Mass Transfers by Fluids in Deformed Metamorphic Rocks. Geodinamica Acta, 1(3), 193–206.PotdevinJ.L., &MarquerD.(1987).Quantitative Methods for the Estimation of Mass Transfers by Fluids in Deformed Metamorphic Rocks.,1(3),193–206.Search in Google Scholar
Putnis, A. (2002). Mineral replacement reactions: from macroscopic observations to microscopic mechanisms. Mineralogical Magazine, 66(5), 689–708.PutnisA.(2002).Mineral replacement reactions: from macroscopic observations to microscopic mechanisms.,66(5),689–708.Search in Google Scholar
Putnis, A. (2009). Mineral Replacement Reactions. Reviews in Mineralogy and Geochemistry, 70(1), 87–124.PutnisA.(2009).Mineral Replacement Reactions.,70(1),87–124.Search in Google Scholar
Putnis, A., & Putnis, C. V (2007). The mechanism of reequilibration of solids in the presence of a fluid phase. Journal of Solid State Chemistry, 180(5), 1783–1786.PutnisA., &PutnisC. V(2007).The mechanism of reequilibration of solids in the presence of a fluid phase.,180(5),1783–1786.Search in Google Scholar
Rüpke, L. H., Morgan, J. P., Hort, M., & Connolly, J. A. (2004). Serpentine and the subduction zone water cycle. Earth and Planetary Science Letters, 223(1-2), 17-34.RüpkeL. H.MorganJ. P.HortM., &ConnollyJ. A.(2004).Serpentine and the subduction zone water cycle.,223(1-2),17-34.Search in Google Scholar
Svensen, H., Planke, S., Malthe-Sørenssen, A., Jamtveit, B., Myklebust, R., Rasmussen Eidem, T., & Rey, S. S. (2004). Release of methane from a volcanic basin as a mechanism for initial Eocene global warming. Nature, 429(6991), 542–545.SvensenH.PlankeS.Malthe-SørenssenA.JamtveitB.MyklebustR.Rasmussen EidemT., &ReyS. S.(2004).Release of methane from a volcanic basin as a mechanism for initial Eocene global warming.,429(6991),542–545.Search in Google Scholar
Tulloch, A.J. (1979). Secondary Ca-Al silicates as low-grade alteration products of granitoid biotite. Contributions to Mineralogy and Petrology, 69(2), 105–117.TullochA.J.(1979).Secondary Ca-Al silicates as low-grade alteration products of granitoid biotite.,69(2),105–117.Search in Google Scholar
Veblen, D., & Ferry, J.M. (1983). A TEM study of the biotitechlorite reaction and comparison with petrologic observations. American Mineralogist, 68, 1160–1168.VeblenD., &FerryJ.M.(1983).A TEM study of the biotitechlorite reaction and comparison with petrologic observations.,68,1160–1168.Search in Google Scholar
Villa, I.M., & Williams, M.L. (2013). Geochronology of metasomatic events. In D.E. Harlov & H. Austrheim (Eds.), Metasomatism and the Chemical Transformation of Rock (pp. 171–202). Springer, Berlin, Heidelberg.VillaI.M., &WilliamsM.L.(2013).Geochronology of metasomatic events.InHarlovD.E., &AustrheimH.(Eds.),(pp.171–202).Springer, Berlin,Heidelberg.Search in Google Scholar
Whitney, D., & Evans, B. (2010). Abbreviations for names of rock-forming minerals. American Mineralogist, 95, 185–187.WhitneyD., &EvansB.(2010).Abbreviations for names of rock-forming minerals.,95,185–187.Search in Google Scholar
Wilamowski, A. (2002). Chloritization and polytypism of biotite in the Łomnica granite, Karkonosze Massif, Sudetes, Poland: Stable isotope evidence. Chemical Geology, 182(2–4), 529–547.WilamowskiA.(2002).Chloritization and polytypism of biotite in the Łomnica granite, Karkonosze Massif, Sudetes, Poland: Stable isotope evidence.,182(2–4),529–547.Search in Google Scholar
Yardley, B.W.D., Rhede, D. & Heinrich, W. (2014). Rates of retrograde metamorphism and their implications for the rheology of the crust: an experimental study. Journal of Petrology, 55(3), 623–641.YardleyB.W.D.RhedeD., &HeinrichW.(2014).Rates of retrograde metamorphism and their implications for the rheology of the crust: an experimental study.,55(3),623–641.Search in Google Scholar
Yuguchi, T., Sasao, E., Ishibashi, M., & Nishiyama, T. (2015). Hydrothermal chloritization processes from biotite in the Toki granite, Central Japan: Temporal variations of the compositions of hydrothermal fluids associated with chloritization. American Mineralogist, 100(5–6), 1134–1152.YuguchiT.SasaoE.IshibashiM., &NishiyamaT.(2015).Hydrothermal chloritization processes from biotite in the Toki granite, Central Japan: Temporal variations of the compositions of hydrothermal fluids associated with chloritization.,100(5–6),1134–1152.Search in Google Scholar
Xiao, B. and Chen, H. (2020). Elemental behavior during chlorite alteration: New insights from a combined EMPA and LA-ICPMS study in porphyry Cu systems. Chemical Geology, 543, 119604.XiaoB.ChenH.(2020).Elemental behavior during chlorite alteration: New insights from a combined EMPA and LA-ICPMS study in porphyry Cu systems.,543,119604.Search in Google Scholar