Prof. Dr. Timm John
Professor für Mineralogie und Petrologie, Freie Universität Berlin.
Akademischer Rat auf Zeit am Institut fur Mineralogy, Universität Münster, Deutschland
Senior postdoctoral researcher at the Centre for Physics of Geological Processes (PGP), Norwegian centre of excellence, University of Oslo. Field coordinator of PGP.
Postdoctoral Fellow. Research project part of SFB 574 “Volatiles and Fluids in Subduction Zones: Climate Feedback and Trigger Mechanism for Natural Disasters“ at University of Kiel, Germany.
Research associate, University of Kiel, Germany
Bohrassistent (traineeship) in einer geologischem Pilotprojekt in Bitterfeld (Germany), Noell Umweltdienste.
Habilitation in Geologie/Mineralogie, Universität Münster, Germany.
Thesis: Physical and chemical processes during the dehydration of subducting oceanic lithosphere: Reactive fluid flow under high-pressure conditions.
Dr. rer. nat., University of Kiel, Germany
Dissertation: Subduction and continental collision in the Lufilian Arc - Zambezi Belt orogen: A petrological, geochemical, and geochronological study of eclogites and whiteschists (Zambia).
Diplom in Geologie, Universität Bremen, Deutschland
Diplomvorprüfung in Geologie, RWTH Aachen, Deutschland
Doktorand, Universität Kiel, Deutschland
Student der Geologie, Universität Bremen, Deutschland
Student der Mineralogie und Geologie, RWTH Aachen, Deutschland
- Stellvertretender Vorsitzender des DVGeo (Dachverband der Geowissenschaften) seit 2019
- Mitgleid der erweiterten Geschäftsführung der DMG (Deutsche Mineralogische Gesellschaft) seit 2017.
- Vorsitzender der Petrologie-Petrophysik Sektion der DMG, 2017-2019.
- Theme coordinator for Goldschmidt 2018 in Boston, USA. Theme “Earth's Lithosphere Formation, Evolution, Recycling, and Subduction” (with M. Brown, F-Y Wu, and C. Till)
- Theme coordinator for GeoBerlin 2015 “DYNAMIC EARTH – from Alfred Wegener to today and beyond”, combined annual meetings of several German Geo-societies and GeoX. Theme A1 Subduction Processes and Continental Collission (with O. Oncken and G. Franz)
- Mitglied im Redaktionkommitee: Lithos, Journal of Metamorphic Geology
- Gastprofessur am École normale supérieure Paris, 04-05/2019
- Gastprofessur an der Université de Lausanne, 06/2019
Gastgeber akademischer Stipendiaten
- Xin Zhong; Alexander von Humboldt stipendiat
- Lisa Kaatz; Elsa Neumann stipendiatin
- Shilei Qiao; China Scholarship Council (CSC) stipendiat
Current Research Topics
Physical and chemical processes during the dehydration of subducting oceanic lithosphere (reactive fluid flow under high-pressure / low-temperature conditions).
During subduction, downgoing plates heat up and their hydrous minerals become progressively unstable and break down to produce water. It is now evident that the released fluids can reach the mantle wedge and cause melting. The most prominent metamorphic reaction occurring in subduction zones is the eclogitization of oceanic crust. It is commonly assumed that the density increase of this reaction makes plate subduction self-sustained. Seismic studies indicate that this transformation happens under non-equilibrium conditions and field evidence points to fluids as a trigger. The details of intra-slab fluid flow are, however, not yet understood. Field evidence points to not yet quantified relationships between reactions, fluid flow, seismicity and mobilization of both major and trace elements. I use a combined field and laboratory based approach to explore the interrelationships of these processes. I investigate how fluids migrate inside slabs (i.e. if fluid migration occurs mainly by distributed porous flow or by channelized fluid flow) and furthermore the interrelation between fluid flow and seismic slip.
Reactive fluid flow and transport of so-called fluid-immobile elements.
The presence of fluids in Earth's crust results in processes that enable significant element mobilization. Metasomatic changes in rocks due to open system reactive fluid flow often cause surprisingly high solubilities and transport rates of so-called fluid-immobile elements, such as HFSE (high field strength elements, e.g., Th, Nb, Ta, Ti) and the REE (rare earth elements). During metasomatism new minerals form which are more stable under the changing physical and chemical conditions. The associated element transport and mineral growth may finally result in economic ore mineralization. We are currently investigating how titanium, tantalum, and niobium (Ti-Nb-Ta) are mobilized and transported and how Nb-Ta are fractionated, even though they are regarded as geochemical identical twins. Metasomatic processes are also interesting with respect to thorium (Th), because this rather immobile element becomes redistributed and concentrated into accessory minerals, while the host rocks experience infiltration of highly oxidizing fluids.
Global chlorine-cycle: halogen concentrations and stable isotopes as tracer for fluid related processes.
The large recycling machines, such as subduction zones and spreading centres, are important for element exchange and transport on Earth. Even though the volatile element chlorine represents an important component of the fluids stored in subducting oceanic lithosphere, the behaviour of chlorine within subduction zones and during the formation of magmas in island arc, in plumes or at spreading ridges is not understood yet. This part of my research is mainly emphasised to establish a conservative trace for subduction zone fluids, i.e. halogen ratios and stable chlorine isotopes (delta37Cl), to identify different fluid sources and to quantify fluid-rock interaction and fluid fluxes. Therefore two main topics are currently in investigation, one is to define the Cl-isotopical signal of the main fluid sources of the deeper fluid cycle, i.e. serpentinite and blueschist dehydration; the other is to investigate how conservative the Cl-isotopes behave during fluid flow and fluid-rock in teraction. I will also try to find "fluid-composition-indicative" minerals to use those as a fluid-probe.
Evolution of craton margins during continent break up and continental collisions (reconstruction of supercontinents and the break up of Gondwana).
Geodynamic processes during orogenesis cause changes in pressure and temperature conditions (P-T conditions), which affect the rocks within an orogen. The reconstruction of the P-T evolution of a metamorphic rock allows to determine the geodynamic causes of metamorphism (e.g., subduction, tectonic thickening, extension during orogenic collapse or rifting, erosion, magmatic underplating). To be able to distinguish between the possible causes for metamorphism and to get a more complete understanding of geodynamic processes the knowledge of the age and the duration of metamorphic events, i.e. the P-T-t path, is essential. My current research is mainly focused on the geodynamic reconstruction of the Neoproterozoic to Cambrian orogens of south central Africa, which are related to the formation of the supercontinent Gondwana. I started to investigate the geodynamic evolution of the Tianshan melange zone (NW China) as a prime example for a cold subduction zone and the continetal margin of Ghana as a prime example for rifting processes along oceanic and continental transform margins
- "Is the depletion of moderately volatile elements in Earth inherited from nebular processes?” research project with doctoral student position; four years funded through DFG grant within the TRR 170 “Late Accretion onto Terrestrial Planets” located at FUB; since 2020-2023; PI: T. John
- "Early-formed rare and unique meteorites and clasts in meteorite breccias” research project with doctoral student position; four years funded through DFG grant within the TRR 170 “Late Accretion onto Terrestrial Planets” located at WWU and FUB; since 2020-2023; PI: T. John
- “Geochemical element mobilization due to poly(hydrogen fluoride) H···F bridged networks” research project with postdoctoral researcher position; four years funded through DFG grant within the SFB “Fluorine-Specific Interactions: Fundamentals and Functions” located at FUB; 2019-2022; PI: T. John
- “Dynamics of rock dehydration on multiple scales” research project with doctoral student position; four years funded through DFG grant within the SFB 1114 “Scaling Cascades in Complex Systems” located at FUB; since 2018-2022; PI: T. John
- “Understanding subduction by linking surface exposures of subducted and exhumed crust to geophysical images of slabs” research project with doctoral student position; three years funded through DFG grant within the SPP 2017 - 4D-MB, since 2017-2020; PI: T. John
- Early-formed, volatile-rich clasts in meteorite breccias: building materials of the terrestrial planets?” research project with doctoral student position; four years funded through DFG grant within the TRR 170 “Late Accretion onto Terrestrial Planets” located at FUB; since 2016-2019; PI: T. John
- “Evolution of zircon chemistry and inclusion paragenesis of I- to S-type granitoids from the Wilson Terrane of northern Victoria Land (Antarctica): Zircon as a record of dynamic continental crust formation”; research project with doctoral student position; three years funded through DFG grant within the SPP 1158 (JO 349/7-1); 2013-2017; PI: T. John
- “Zooming in between plates: deciphering the nature of the plate interface in subduction zones”; Partner in EU funded Marie Curie ITN; 2013-2017; PI: T. John
- “Timing and rates of fluid release during the dehydration of subducting oceanic crust: reactive fluid flow under high-pressure conditions”; research project with doctoral student position; three years funded through DFG grant (JO 349/5-1); since 2011-2017; PI: T. John
- “Halogen concentrations and stable Cl isotopes in apatite as a fluid probe: mapping regional-scale fluid pulses by Cl-isotopes”; research project with doctoral student position; three years funded through DFG grant (JO 349/3-1); 2010-2015; PI: T. John“
- Decoding the transient porosity and permeability evolution during fluid-rock interaction” Research at Advanced Photon Source (Argonne-Chicago, USA) GUP 35213; Since 2013-2014, Co-PI: T. John
The current selection of the ten highlight papers:
*denotes either first author being a student of T. John or T. John is corresponding author
*Beinlich, A., John, T., Vrijmoed, J.C., Tominaga, M., Magna, T., Podladchikov, Y. (2020). Instantaneous rock transformations in the deep crust driven by reactive fluid flow. Nature Geoscience, http://doi.org/10.1038/s41561-020-0554-9
Bedford, J., Moreno, M., Deng, Z., Oncken, O., Schurr, B., John, T., Baez, J.C., Bevis, M. (2020). Months-Long thousand-km-scale wobbling before great subduction earthquakes. Nature.
*Li, J.-L., Schwarzenbach, E.M., John, T., Ague, J. J., Huang, F., Gao, J., Klemd, R., Whitehouse, M. & Wang, X.-S. (2020). Uncovering and quantifying the subduction zone sulfur cycle from the slab perspective. Nature Communications, 1–12. http://doi.org/10.1038/s41467-019-14110-4
Chen, S., Hin, R.C., John, T., Brooker, R., Bryan, B., Niu, Y. & Elliott, T. (2019). Molybdenum systematics of subducted crust record reactive fluid flow from underlying slab serpentine dehydration. Nature Communications, 1–9. http://doi.org/10.1038/s41467-019-12696-3
*Taetz, S., John, T., Bröcker, M., Spandler, C. & Stracke, A. (2018). Fast intraslab fluid-flow events linked to pulses of high pore fluid pressure at the subducted plate interface. Earth and Planetary Science Letters 482, 33–43.
*Plümper, O., John, T., Podladchikov, Y.Y. , Vrijmoed, J.C. & Scambelluri, M. (2017). Fluid escape from subduction zones controlled by channel-forming reactive porosity. Nature Geoscience 10,150–156.
John, T., Gussone, N., Podladchikov, Y.Y., Bebout, G., Dohmen, R., Halama, R., Klemd, R., Magna, T. & Seitz, M. (2012). Volcanic arcs fed by rapid pulsed fluid flow through subducting slabs. Nature Geoscience, 5, 489-492.
Putnis, A. & John, T. (2010). Replacement processes in the Earth’s crust. Elements, 6, 159-164.
John, T., Medvedev, S., Rüpke, L.H., Podladchikov, Y., Andersen, T.B. & Austrheim, H. (2009). Generation of intermediate-depth earthquakes by self-localizing thermal runaway. Nature Geoscience, 2, 137-140.
*Gao, J., John, T., Klemd, R. & Xiong, X. (2007). Mobilisation of Ti-Nb-Ta during subduction: insights from rutile precipitates in eclogite-facies segregations and veins (Tianshan, NW China). Geochimica et Cosmochimica Acta, 71, 4974-4996.
Publikationen (peer reviewed)
- Beinlich, A., John, T., Vrijmoed, J. C., Tominaga, M., Magna, T., Podladchikov, Y. Y. Instantaneous rock transformations in the deep crust driven by reactive fluid flow. Nature Geocience, http://doi.org/10.1038/s41561-020-0554-9
- Peters, D., Pettke, T., John, T., Scambelluri, M. The role of brucite in water and element cycling during serpentinite subduction – Insights from Erro Tobbio (Liguria, Italy), Lithos 360, https://doi.org/10.1016/j.lithos.2020.105431
Urann, B. M., Le Roux, V., John, T., Beaudoin, G. M., Barnes, J. D. The distribution and abundance of halogens in eclogites: An in situ SIMS perspective of the Raspas Complex (Ecuador), American Mineralogist 105: 307-318, https://doi.org/10.2138/am-2020-6994
- Groß, P., Handy, M. R., John, T., Pestal, G., Pleuger, J. Crustal-Scale Sheath Folding at HP Conditions in an Exhumed Alpine Subduction Zone (Tauern Window, Eastern Alps), Tectonics 39
- Bayet, L., Agard, P., John ,T., Menneken, M., Tan, Z., Gao, J. Tectonic evolution od the Tianshan Akeyazi metamorphic complex (NW China), Lithos, https://doi.org/10.1016/j.lithos.2019.105273
- Patzek, M., Hoppe, P., Bischoff, A., Visser, R., John, T. Hydrogen isotopic composition of CI- and CM-like clasts from meteorite breccias - Sampling unknown sources of carbonaceous condrite materials, Geochemica et Cosmochemica Acta 272, p. 177-197, https://doi.org/10.1016/j.gca.2019.12.017
- Li, J.-L., Schwarzenbach, E.M., John, T., Ague, J. J., Huang, F., Gao, J. Klemd, R., Whitehouse, M. J., Wang, X.-S. Uncovvering and quantifying the subduction zone sulfur cycle from the slab perspective, Nature Communications 11, p. 1-12
- Su, W., Schwarzenbach, E. M., Chen, L., Li, Y., John, T., Gao, J., Chen, F., Hu, X., Suphur isotope compositions of pyrite from high-pressure metamorphic rocks and related veins (SW Tianshan, China): Implications for the sulphur cycle in subduction zones, Lithos 348, p. 105212, https://doi.org/10.1016/j.lithos.2019.105212
- Incel, S., Schubnel, A., Renner, J., John, T., Labrousse, L., Hilairet, N., Freeman, H., Wang, Y., Renard, F., Jamtveit, B. Experimental evidence for wall-rock pulverization during dynamic rupture at ultra-high pressure conditions, Earth and Planetary Science Letters 528, p. 115832, https://doi.org/10.1016/j.epsl.2019.115832
- Chen, S., Hin, R.C., John ,T., Brooker, R., Bryan, Niu, Y., Elliott, T. Molybdenum systematics of subducted crust record reactive fluid flow from underlying slab serpentine dehydration, Nature Communications 10, 4773, https://doi.org/10.1038/s41467-019-12696
- Zertani, S., John, T., Tilmann, F., Motra, H.B., Keppler, R., Andersen, T.B., Labrousse, L. Modification of the seismic proerties of subduction continental crust by eclogitization and deformation processes, Journal of Geophysical Research - Solid Earth, doi.org/10.1029/2019JB017741
- Sippl, C., Schurr, B., John, T., Hainzl, S. Filling the gap in a double seismic zone: Intraslab seismicity in Northern Chile, Lithos 346, p. 105155, https://doi.org/10.1016/j.lithos.2019.105155
- Visser, R., John, T., Patzek, M., Bischoff, A., Whitehouse, M. J. Sulphur isotope study of sulfides in CI, CM, C2ung Chondrites and volatile-rich clasts - Evidence for different generations and reservoirs of sulfide formation, Geochemica et Cosmochemica Acta 261, p. 210-223, https://doi.org/10.1016/j.gca.2019.06.046
- Tan, Z., Agard, P., Monié, P., Gao, J., John, T., Bayet, L., Jiang, T., Wang, X.-S., Hong, T., Wan, B., Caron, B. Architecture ant P-T-deformation-time evolution of the Chinese SW-Tianshan HP/UHP complex: Implications for subduction dynamics, Earth-Science Reviews 197, p. 102894, https://doi.org/10.1016/j.earscirev.2019.102894
- Guo, S., Zhao, K., John, T., Tang, P., Chen, Y., Su, B. Metasomatic flow of metacarbonate-derived fluids carrying isotopically heavy boron in continental subduction zones: Insights from tourmaline-bearing ultra-high pressure eclogites and veins (Dabie terrane, eastern China). Geochimica Et Cosmochimica Acta 253, 159–200.
- Zertani, S., Labrousse, L., John, T., Andersen, T.B., Tilmann, F. The Interplay of Eclogitization and Deformation During Deep Burial of the Lower Continental Crust—A Case Study From the Bergen Arcs (Western Norway). Tectonics 38.
- Incel, S., Labrousse, L., Hilairet, N., John, T., Gasc, J., Shi, F., Wang, Y., Andersen, T. B., Renard, F., Jamtveit, B., Schubnel, A. Reaction-induced embrittlement of the lower continental crust. Geology 47 (3), 235-238.
- Shu, Y., Nielsen, S. G., Marschall, H. R., John, T., Blusztajn, J., Auro, M. Closing the loop: Subducted eclogites match thallium isotope compositions of ocean island basalts. Geochimica et Cosmochimica Acta 250, 130-148.
- Roszjar, J., Whitehouse, M.J., Terada, K., Fukuda, K., John, T., Bischoff, A., Morishita, Y., Hiyagon, H. Chemical, microstructural and chronological record of phosphates in the Ksar Ghilane 002 enriched shergottite. Geochimica et Cosmochimica Acta 245, 385–405.
- Bayet, L., John, T., Agard, P., Gao, J., Li, J. L. Massive sediment accretion at∼ 80 km depth along the subduction interface: Evidence from the southern Chinese Tianshan. Geology 46 (6), 495-498.
- Liebmann, J., Schwarzenbach, E. M., Früh-Green, G. L., Boschi, C., Rouméjon, S., Strauss, H., Wiechert, U., John, T. Tracking Water-Rock Interaction at the Atlantis Massif (MAR, 30°N) Using Sulfur Geochemistry. Geochemistry, Geophysics, Geosystems, 19.
- Bloch, W., John, T., Kummerow, J., Salazar, P., Krüger, O. S., Shapiro, S. A. Watching dehydration: Seismic Indication for Transient Fluid Pathways in the Oceanic Mantle of the Subducting Nazca Slab. Geochemistry, Geophysics, Geosystems, 19.
- Visser, R., John, T., Menneken, M., Patzek, M., Bischoff, A. Temperature constraints by Raman spectroscopy of organic matter in volatile-rich clasts and carbonaceous chondrites. Geochimica et Cosmochimica Acta 241, 38–55.
- Patzek, M., Bischoff, A., Visser, R., John, T. Mineralogy of volatile-rich clasts in brecciated meteorites. Meteoritics & Planetary Science, 1–22.
- Taetz, S., John, T., Bröcker, M., Spandler, C., Stracke, A. Fast intraslab fluid-flow events linked to pulses of high pore fluid pressure at the subducted plate interface. Earth and Planetary Science Letters 482, 33–43.
- Macente, A., Fusseis, F., Menegon, L., Xiao, X, John, T. The strain‐dependent spatial evolution of garnet in a high‐P ductile shear zone from the Western Gneiss Region (Norway): a synchrotron X‐ray microtomography study. Journal of Metamorphic Geology 35 (5), 565-583.
- Li, J.L., John, T., Gao, J., Klemd, R., Wang, X.S. Subduction channel fluid–rock interaction and mass transfer: Constraints from a retrograde vein in blueschist (SW Tianshan, China). Chemical Geology, 456, 28-42.
- Tan, Z., Agard, P., Gao, J., John T., Li, J. L., Jiang, T., Bayet, L., Wang, X., Zhangg, X. P-T-time-isotopic evolution of coesite-bearing eclogites: Implications for exhumation processes in SW Tianshan. Lithos 281, 1-25.
- Halama, R., Bebout G., Marschall H., John, T. Fluid-induced breakdown of white mica controls nitrogen transfer during fluid-rock interaction in subduction zones. International Geology Review, 59, 702–720.
- Peters, D., Bretscher, A., John, T., Scambelluri, M., Pettke, T. Fluid-mobile elements in serpentinites: Constraints on serpentinisation environments and element cycling in subduction zones. Chemical Geology, 466, 654-666.
- Plümper, O., John, T., Podladchikov, Y. Y. , Vrijmoed, J. C. & Scambelluri, M. Fluid escape from subduction zones controlled by channel-forming reactive porosity. Nature Geoscience, 10,150–156.
- Manzini M., Bouvier A.-S., Barnes J. D., Bonifacie M., Rose-Koga E. F., Ulmer P., Métrich N., Bardoux G., Williams J., Layne G. D., Straub S., Baumgartner L. P., John T. SIMS chlorine isotope analyses in melt inclusions from arc settings. Chemical Geology, 449, 112-122.
- Bellucci, J. J., Whitehouse, M. J., John, T., Nemchin, A. A., Snape, J. F., Bland, P. A., & Benedix, G. K. Halogen and Cl isotopic systematics in Martian phosphates: Implications for the Cl cycle and surface halogen reservoirs on Mars. Earth and Planetary Science Letters, 458, 192–202.
- Incel, S., Hilairet, N., Labrousse, L., John, T., Deldicque, D., Ferrand, T., et al. Laboratory earthquakes triggered during eclogitization of lawsonite-bearing blueschist. Earth and Planetary Science Letters, 459, 320–331.
- Sarafian, A. R., John, T., Roszjar, J., & Whitehouse, M. J. Chlorine and hydrogen degassing in Vesta’s magma ocean. Earth and Planetary Science Letters, 459, 311–319.
- Halama, R., Bebout, G. E., Marschall, H. R., & John, T. Fluid-induced breakdown of white mica controls nitrogen transfer during fluid–rock interaction in subduction zones. International Geology Review, 1–19.
- Li, J.-L., Gao, J., Klemd, R., John, T., & Wang, X.-S. Redox processes in subducting oceanic crust recorded by sul de‐bearing high‐pressure rocks and veins (SW Tianshan, China). Contributions to Mineralogy and Petrology, 171:72.
- Raith, M. M., Brandt, S., Sengupta, P., Berndt, J., John, T., & Srikantappa, C. Element Mobility and Behaviour of Zircon during HT Metasomatism of Ferroan Basic Granulite at Ayyarmalai, South India: Evidence for Polyphase Neoarchaean Crustal Growth and Multiple Metamorphism in the Northeastern Madurai Province. Journal of Petrology, 57, 1729–1774.
- Taetz, S., John, T., Bröcker, M., & Spandler, C. Fluid–rock interaction and evolution of a high-pressure/low- temperature vein system in eclogite from New Caledonia: insights into intraslab fluid flow processes. Contributions to Mineralogy and Petrology, 171:90.
- Meyer, M., Klemd, R., John, T., Gao, J. & Menneken, M. An (in-)coherent metamorphic evolution of high-pressure eclogites and their host rocks in the Chinese southwest Tianshan. Journal of Metamorphic Geology, 34, 121-146.
- Li, J.-L., Klemd, R., Gao, J., & John, T. Poly-cyclic metamorphic evolution of eclogite: evidence for multistage burial–exhumation cycling in a subduction channel. Journal of Petrology, 57, 119–146.
- Kusebauch, C., John, T., Barnes, J., Klügel, A., & Austrheim, H. Halogen element and stable chlorine isotope fractionation caused 1 by fluid-rock interaction (Bamble sector SE Norway). Journal of Petrology, 56, 299-324.
- Kusebauch, C., John, T., Whitehouse, M. & Engvik, A. Apatite as probe for the halogen composition of metamorphic fluids (Bamble Sector SE Norway). Contributions to Mineralogy and Petrology, 170:34.
- Kusebauch, C., John, T., Whitehouse, M., Klemme, S. & Putnis, A. Distribution of halogens between fluid and apatite during fluid-mediated replacement processes. Geochimica et Cosmochimica Acta. 170, 225-246.
- Collins, N., Bebout, G., Angiboust, S., Agard, P., Scambelluri, M., Crispini, L. & John, T. Subduction zone metamorphic pathway for deep carbon cycling: II. Evidence from HP/UHP metabasaltic rocks and ophicarbonates. Chemical Geology, 412, 132-150.
- Farber, K., Caddick, M. & John, T. Controls on solid-phase inclusion during porphyroblast growth: insights from the Barrovian sequence (Scottish Dalradian). Contributions to Mineralogy and Petrology, 168, 1-17.
- Pollok , K., Heidelbach, F., John, T., & Langenhorst. Spherulitic omphacite in pseudotachylytes: Microstructures related to fast crystal growth from seismic melt at eclogite-facies conditions. Chemie der Erde, 74, 407–418.
- Halama, R., Bebout, G., John, T. & Scambelluri, M. Nitrogen recycling in subducted mantle rocks and implications for the global nitrogen cycle. International Journal of Earth Science, 103, 2081-2099.
- Majumdar, A., King, H., John, T., Kusebauch, C. & Putnis A. Pseudomorphic replacement of diopside during interaction with (Ni,Mg)Cl2 aqueous solutions: Implications for Ni-enrichment mechanism in talc- and serpentine-type phases. Chemical Geology, 380, 27-40.
- Jonas, L., John, T., King, H., Geisler, T. & Putnis, A. The role of grain boundaries and transient porosity in rocks as fluid pathways for reaction front propagation. Earth and Planetary Science Letters, 386, 64-74.
- Klemme, S., John, T., Wessels, M., Kusebauch, C., Berndt, J., Rohrbach, A. & Schmid-Beurmann, P. Synthesis of trace element bearing single crystals of Chlor-Apatite (Ca5(PO4)3Cl) using the flux growth method. Chemistry Central Journal, 7, article number 56.
- Vrijmoed, J.C., Austrheim, H., John, T., Hin, R., Davies, G.R. & Corfu, F. Metasomatism in the ultra-high pressure Svartberget garnet-peridotite (Western Gneiss Region, Norway): Implications for the transport of crust-derived fluids within the mantle. Journal of Petrology, 54, 1815-1848.
- Jonas, L. John, T. & Putnis. A. Influence of temperature and Cl on the hydrothermal replacement of calcite by apatite and the development of porous microstrcutures. American Mineralogist, 98, 1516-1525.
- Li, J.-L., Gao, J., John, T., Klemd, R., & Su, W. Fluid-mediated metal transport in subduction zones and its link to arc-related giant ore deposits: Constraints from a sulfide-bearing HP vein in lawsonite eclogite (Tianshan, China). Geochimica et Cosmochimica Acta, 120, 326–362.
- John, T., Gussone, N., Podladchikov, Y.Y., Bebout, G., Dohmen, R., Halama, R., Klemd, R., Magna, T. & Seitz, M. Volcanic arcs fed by rapid pulsed fluid flow through subducting slabs. Nature Geoscience, 5, 489-492.
- Herms, P., John, T., Bakker, R.J. & Schenk, V. Evidence for channelized external fluid flow and element transfer in subducting slabs (Raspas Complex, Ecuador). Chemical Geology, 310-311, 79-96.
- van der Straaten, F., Halama, R., John, T., Schenk, V., Hauff, F. & Andersen, N. Tracing the effects of high-pressure metasomatic fluids and seawater alteration in blueschist-facies overprinted eclogites: Implications for subduction channel processes. Chemical Geology, 292-293, 69-87.
- John, T., Scambelluri, M., Frische, M., Barnes, J.D. & Bach, W. Dehydration of subducting serpentinite: implications for halogen mobility in subduction zones and the deep halogen cycle. Earth and Planetary Science Letters, 308, 65-76.
- Smit, M., Scherer, E., John, T. & Janssen, A. Creep of garnet in eclogite: mechanisms and implications. Earth and Planetary Science Letters, 311, 411-419.
- Klemd, R., John, T., Scherer, E.E., Rondenay, S. & Gao, J. Change in dip of subducting slabs at greater depths: petrological and geochronological evidence from HP-UHP rocks (Tianshan, NW-China). Earth and Planetary Science Letters, 310, 9-20.
- John, T., Klemd, R., Klemme, S., Pfänder, J., Hoffmann, J.E. & Gao, J. Nb-Ta fractionation by partial melting at the titanite-rutile transition. Contributions to Mineralogy and Petrology, 161, 35-45.
- Meyer, M., John, T., Brandt, S. & Klemd, R. Trace element composition of rutile and the application of Zr-in-rutile thermometry to UHT metamorphism (Epupa Complex, NW Namibia). Lithos, 126, 388-401.
- Raufaste, C., Jamtveit, B., John, T., Meakin, P. & Dysthe, D.K. The mechanism of porosity formation during solvent-mediated phase transformations. Proceedings of the Royal Society A, 467, 1408-1426.
- Halama, R., John, T., Herms, P., Hauff, F. & Schenk, V. A stable (Li, O) and radiogenic (Sr, Nd) isotope perspective on metasomatic processes in a subducting slab. Chemical Geology 281, 151-166.
- John, T., Layne, G., Haase, K. & Barnes, J.D. Chlorine isotope evidence for crustal recycling into the Earth´s mantle. Earth and Planetary Science Letters, 298, 175-182.
- Putnis, A. & John, T. Replacement processes in the Earth’s crust. Elements, 6, 159-164.
- Beinlich, A., Klemd, R., John, T. & Gao, J. Trace-element mobilization during Ca-metasomatism along a major fluid conduit: eclogitization of blueschists as a consequence of fluid-rock interaction. Geochimica et Cosmochimica Acta, 74, 1892-1922.
- John, T., Scherer, E.E., Schenk, V., Herms, P., Halama, R. & Garbe-Schönberg, D. Subducted seamounts in an eclogite-facies ophiolite sequence: The Andean Raspas Complex, SW Ecuador. Contributions to Mineralogy and Petrology, 159, 265-284.
- Halama, R., Bebout, G. E., John, T. & Schenk, V. Nitrogen recycling in subducted oceanic lithosphere: the record in high- and ultrahigh pressure metabasaltic rocks. Geochimica et Cosmochimica Acta. 74, 1636-1652.
- John, T., Medvedev, S., Rüpke, L.H., Podladchikov, Y., Andersen, T.B. & Austrheim, H. Generation of intermediate-depth earthquakes by self-localizing thermal runaway. Nature Geoscience, 2, 137-140.
- Adamuszek, M., John, T., Dabrowski, M., Podladchikov, Y.Y. & Gertisser, R. Assimilation and diffusion during xenolith-magma interaction: A case study of the Variscan Karkonosze granite, Bohemian Massif. Mineralogy and Petrology, 97, 203-222.
- Schmidt, A., Weyer, S., John, T. & Brey, G.P. HFSE systematics of rutile-bearing eclogites: New insights into subduction zone processes and implications for the Earth's HFSE budget. Geochimica et Cosmochimica Acta, 73, 455-468.
- John, T., Klemd, R., Gao, J. & Garbe-Schönberg, C-D. Trace-element mobilization in slabs due to non steady-state fluid-rock interaction: constraints from an eclogite-facies transport vein in blueschist (Tianshan, China). Lithos, 103, 1-24.
- van der Straaten, F., Schenk, V., John, T. & Gao, J. Blueschist-facies rehydration of eclogites: implications for subduction channel fluid-rock interaction from the Tianshan, NW China. Chemical Geology, 255, 195-219.
- Iyer, K., Austrheim, H., John, T. & Jamtveit, B. Serpentinization of the oceanic lithosphere and some geochemical consequences: Constraints from the Leka Ophiolite Complex, Norway. Chemical Geology, 249, 66-90.
- Zack, T. & John, T. An evaluation of reactive fluid flow and trace-element mobility in subducting slabs. Chemical Geology, 239, 199-216.
- Gao, J., John, T., Klemd, R. & Xiong, X. Mobilisation of Ti-Nb-Ta during subduction: insights from rutile precipitates in eclogite-facies segregations and veins (Tianshan, NW China). Geochimica et Cosmochimica Acta, 71, 4974-4996.
2006 und davor
- John, T. & Schenk, V, 2006. Interrelations between intermediate-depth earthquakes and fluid flow within subducting oceanic plates: constraints from eclogite-facies pseudotachylytes. Geology, 34, 557-560.
- Xiong X., John T., Gao J., Klemd R. & Huang D., 2006. Trace element mobilization in subducted slabs: Constraints on an eclogite-facies transport vein from the western Tianshan, NW China. Acta Geologica Sinica, 80, 53-60.
- John, T., Scherer, E., Haase, K. & Schenk, V., 2004. Trace element fractionation during fluid-induced eclogitization in a subducting slab: trace element and Lu-Hf / Sm-Nd isotope systematics. Earth and Planetary Science Letters, 227, 441-456.
- John, T., Schenk, V., Mezger, K. & Tembo, F., 2004. Timing and P-T evolution of whiteschist metamorphism in the Lufilian Arc-Zambezi Belt orogen (Zambia): implications to the Gondwana assembly. The Journal of Geology, 112, 71-90.
- John, T. & Schenk, V., 2003. Partial eclogitisation of gabbroic rocks in a late Precambrian subduction zone (Zambia): prograde metamorphism triggered by fluid infiltration. Contributions to Mineralogy and Petrology, 146, 174-191.
- John, T., Schenk, V., Haase, K., Scherer, E. & Tembo, F., 2003. Evidence for a Neoproterozoic ocean in south central Africa from MORB-type geochemical signatures and P-T estimates of Zambian eclogites. Geology, 31, 243-246.
- John, T, Klemd, R., Hirdes, W. & Loh, G., 1999. The metamorphic evolution of the Paleoproterozoic (Birimian) volcanic Ashanti belt (Ghana, West Africa). Precambrian Research, 98, 11-30.
- John, T., Klemd, R., Hirdes, W. & Loh, G., 1998. The metamorphic evolution of the Paleoproterozoic (Birimian) gold-bearing Ashanti volcanic belt, West Africa. Zeitschrift für Angewandte Geologie, 44, 108-110.