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Artykuły w czasopismach na temat "Metamorphic reaction"
Degeling, H., S. Eggins i D. J. Ellis. "Zr budgets for metamorphic reactions, and the formation of zircon from garnet breakdown". Mineralogical Magazine 65, nr 6 (grudzień 2001): 749–58. http://dx.doi.org/10.1180/0026461016560006.
Pełny tekst źródłaRidley, John. "Modelling of the relations between reaction enthalpy and the buffering of reaction progress in metamorphism". Mineralogical Magazine 50, nr 357 (wrzesień 1986): 375–84. http://dx.doi.org/10.1180/minmag.1986.050.357.03.
Pełny tekst źródłaUrueña, Cindy L., Charlotte Möller i Anders Plan. "Metamorphic titanite–zircon pseudomorphs after igneous zirconolite". European Journal of Mineralogy 35, nr 5 (19.09.2023): 773–88. http://dx.doi.org/10.5194/ejm-35-773-2023.
Pełny tekst źródłaTettelaar, Tanya, i Aphrodite Indares. "Granulite-facies regional and contact metamorphism of the Tasiuyak paragneiss, northern Labrador: textural evolution and interpretation". Canadian Journal of Earth Sciences 44, nr 10 (1.10.2007): 1413–37. http://dx.doi.org/10.1139/e07-029.
Pełny tekst źródłaXiao, Ling-Ling, i Min-Hua Chen. "Metamorphic Age Comparison and Its Implications between the Zuoquan and Zanhuang Complexes in the Central North China Craton, Based on LA-ICP-MS Zircon U–Pb Dating". Minerals 9, nr 12 (13.12.2019): 780. http://dx.doi.org/10.3390/min9120780.
Pełny tekst źródłaDutta, Upama, Ayan Kumar Sarkar, Sadhana M. Chatterjee, Anirban Manna, Alip Roy i Subhrajyoti Das. "Petrological implications of element redistribution during metamorphism: insights from meta-granite of the South Delhi Fold Belt, Rajasthan, India". Geological Magazine 159, nr 5 (23.02.2022): 735–60. http://dx.doi.org/10.1017/s0016756821001345.
Pełny tekst źródłaMcElhinney, Tara R., Tim J. Dempster i Peter Chung. "The influence of microscale lithological layering and fluid availability on the metamorphic development of garnet and zircon: insights into dissolution–reprecipitation processes". Mineralogical Magazine 86, nr 1 (13.12.2021): 9–26. http://dx.doi.org/10.1180/mgm.2021.97.
Pełny tekst źródłaLazzarotto, Manuele, David R. M. Pattison, Simon Gagné i Paul G. Starr. "Metamorphic and structural evolution of the Flin Flon – Athapapuskow Lake area, west-central Manitoba". Canadian Journal of Earth Sciences 57, nr 11 (listopad 2020): 1269–88. http://dx.doi.org/10.1139/cjes-2019-0136.
Pełny tekst źródłaMitchell, J. N. "A Scanning Electron Microscopic study of hematite inclusions in cordierite porphyroblasts". Proceedings, annual meeting, Electron Microscopy Society of America 44 (sierpień 1986): 680–981. http://dx.doi.org/10.1017/s0424820100144796.
Pełny tekst źródłaPowell, W. G., D. M. Carmichael i C. J. Hodgson. "Conditions and timing of metamorphism in the southern Abitibi greenstone belt, Quebec". Canadian Journal of Earth Sciences 32, nr 6 (1.06.1995): 787–805. http://dx.doi.org/10.1139/e95-067.
Pełny tekst źródłaRozprawy doktorskie na temat "Metamorphic reaction"
Corona, Juan Carlos. "An experimental investigation of the reaction glaucophane + 2 quartz = 2 albite + talc /". Diss., Online access via UMI:, 2005.
Znajdź pełny tekst źródłaKleine, Barbara I. "How do metamorphic fluids move through rocks? : An investigation of timescales, infiltration mechanisms and mineralogical controls". Doctoral thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-115172.
Pełny tekst źródłaAt the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 2: Manuscript. Paper 3: Manuscript. Paper 4: Manuscript.
Mansard, Nicolas. "The role of metamorphic reactions for strain localization in the middle and lower crust : Insights from field observations and deformation experiments". Thesis, Orléans, 2019. http://www.theses.fr/2019ORLE3103.
Pełny tekst źródłaShear zones arise from strain localization into rocks of the crust and uppermost mantle during deformation of the lithosphere. By accommodating a large amount of strain, these shear zones have a direct control on rheology and dynamics of the lithosphere. Based on field observations and deformation experiments, this study aims at extending the current knowledge about the rheological behavior and the development of shear zones. In this study, we highlight that the rheological behavior of polyphase materials is extremely sensitive to their mineralogical composition and that small chemical variations can initiate strain localization – even at small shear strain - and induce large differences in resistance. Our results also show the ability of deformation to enhance mineral reactions, nucleation, the development of fine-grained mixed zones and, conversely, how such an evolution in microstructures eventually results in strain localization and weakening of polyphase aggregates. Phase compositions, in as much they control the reactivity, play a first-order role on both the initiation of weakening but also on the long-term evolution and strength of shear zones. Overall, our study illustrates that the rheology of rocks cannot be summarized as being controlled by monophase materials. In order to further use the rheological models as a predictive tool for lithospheric rheology, it seems essential to take into account both the complexity of regional structures (such as shear zone areas) and the complete nature of rocks that compose them, including the rheology of polyphase material in presence—or in absence—of feedback between deformation and reactions
Cui, Xiaojun. "Numerical modeling of reactive fluid flow in the Notch Peak contact metamorphic aureole, Utah /". free to MU campus, to others for purchase, 2002. http://wwwlib.umi.com/cr/mo/fullcit?p3060092.
Pełny tekst źródłaWorden, R. H. "Transmission electron microscopy of metamorphic reactions". Thesis, University of Manchester, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.234381.
Pełny tekst źródłaSonnet, Manon. "Signature géophysique du panneau plongeant alpin : analogues de terrain et modèles directs". Electronic Thesis or Diss., Sorbonne université, 2023. http://www.theses.fr/2023SORUS595.
Pełny tekst źródłaRecent geophysical images in the Alps show a distinctive seismic signature of the top of the crustal dipping panel at 40 km depth. A sharp increase in S-wave velocity is correlated with a high probability of interface contrast in tomography and negative conversion in stacked receiver- function data. The aim of this thesis is to assess if changes in the mineralogy and textural properties of the lower continental crust can explain this seismic signature. To this end, we calculated bulk seismic velocity variations, generated by mineralogical changes during burial of rocks representative of the European lower crust along pressure- temperature profiles typical of convergence zones. We studied the evolution of the macroscopic anisotropy of the same rocks as a function of pressure and temperature, using direct measurements. These measurements are compared with anisotropy calculations commonly performed from thin- section crystallographic orientation maps. The ultimate aim of these exercises is to understand which properties control the effective seismic velocities of rocks at kilometer scale. Finally, we have attempted to detect the anisotropy of rocks at this latter scale in receiver-function data from their harmonic decomposition. We show that the transformation of rocks from amphibolite to high-pressure granulite facies explains the increase in velocity of the tomographic model, and that this front is shifted by around ten kilometers along the slab, compared with thermodynamic predictions. Using thermokinetic modelling of convergence zones, we evaluate the thermal profile of the dipping panel during the transition from subduction to collision, and explain this offset by kinetic effects. Direct measurements compared with anisotropy calculations indicate that the expected difference between intrinsic and effective anisotropy is greater in amphibolite facies rocks, where layering and CPO are enhanced, than in granulite facies rocks, where anisotropy results mainly from intrinsic anisotropy. At kilometer scale, amphibolite-to-granulite transformation is likely to be accompanied by a decrease in anisotropy in addition to an increase in velocity. Through harmonic decomposition, we show that the reduced visibility of the Moho, at stations above the dipping panel, is to the benefit of highlighting a fast intra-slab direction oriented perpendicular to its dip. Since this transformation is visible both in the receiver-function data and in the tomography models, we deduce that the thickness of the reaction front is of the order of a kilometer
Marchildon, Marie-France Nathalie. "Petrologic studies of process interactions in metamorphic systems, deformation and metamorphism in the Selkirk Allochthon orogenic wedge : and feedback mechanisms during reactive fluid flow". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0018/NQ48658.pdf.
Pełny tekst źródłaDoyle, John Andrew. "Experimental study of the effect of H2O-CO2-NaCl fluid immiscibility on the reaction calcite + quartz + rutile = sphene + CO2 at 2 KBAR". Thesis, Virginia Polytechnic Institute and State University, 1989. http://hdl.handle.net/10919/53208.
Pełny tekst źródłaMaster of Science
Lamadrid, De Aguinaco Hector M. "Geochemistry of fluid-rock processes". Diss., Virginia Tech, 2016. http://hdl.handle.net/10919/71350.
Pełny tekst źródłaPh. D.
Pollard, Brittney Maryah. "Reactivation of fractures as discrete shear zones from fluid enhanced reaction softening, Harquahala metamorphic core complex, west-central Arizona". Thesis, 2014. http://hdl.handle.net/2152/25744.
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Książki na temat "Metamorphic reaction"
International, Geological Congress (29th 1992 Kyoto Japan). Metamorphic reaction: Kinetics and mass transfer. Utrecht: VSP, 1994.
Znajdź pełny tekst źródłaThompson, Alan Bruce, i David C. Rubie, red. Metamorphic Reactions. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5066-1.
Pełny tekst źródłaFyfe, W. S. Metamorphic reactions and metamorphic facies. Ann Arbor, MI: University Microfilms International, 1985.
Znajdź pełny tekst źródła1947-, Thompson Alan Bruce, Rubie David C i Bayly M. Brian 1929-, red. Metamorphic reactions: Kinetics, textures, and deformation. New York: Springer-Verlag, 1985.
Znajdź pełny tekst źródła(Editor), P. J. Treloar, i P. O'Brien (Editor), red. What Drives Metamorphism and Metamorphic Reactions (Geological Society Special Publication). Geological Society Publishing House, 1998.
Znajdź pełny tekst źródłaAlan Bruce Thompson Cees van Dam. Metamorphic Reactions: Kinetics, Textures, and Deformation. Springer, 2011.
Znajdź pełny tekst źródłaBrodie, K. H., B. Bayly, D. C. Rubie i A. B. Thompson. Metamorphic Reactions: Kinetics, Textures, and Deformation. Springer, 2012.
Znajdź pełny tekst źródłaVernon, R. H. Metamorphic Processes: Reactions and Microstructure Development. Springer London, Limited, 2012.
Znajdź pełny tekst źródłaThompson, Alan Bruce. Metamorphic Reactions: Kinetics, Textures and Deformation (Advances in Physical Geochemistry, Vol 4). Springer, 1985.
Znajdź pełny tekst źródłaCzęści książek na temat "Metamorphic reaction"
Ridley, J. "The Effect of Reaction Enthalpy on the Progress of a Metamorphic Reaction". W Metamorphic Reactions, 80–97. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5066-1_3.
Pełny tekst źródłaFerry, J. M. "Reaction Progress: A Monitor of Fluid—Rock Interaction during Metamorphic and Hydrothermal Events". W Advances in Physical Geochemistry, 60–88. New York, NY: Springer New York, 1986. http://dx.doi.org/10.1007/978-1-4612-4896-5_3.
Pełny tekst źródłaCarpenter, M. A., i A. Putnis. "Cation Order and Disorder during Crystal Growth: Some Implications for Natural Mineral Assemblages". W Metamorphic Reactions, 1–26. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5066-1_1.
Pełny tekst źródłaWintsch, R. P. "The Possible Effects of Deformation on Chemical Processes in Metamorphic Fault Zones". W Metamorphic Reactions, 251–68. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5066-1_10.
Pełny tekst źródłaBayly, B. "Deformation with Simultaneous Chemical Change: The Thermodynamic Basis". W Metamorphic Reactions, 269–77. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5066-1_11.
Pełny tekst źródłaRubie, D. C., i A. B. Thompson. "Kinetics of Metamorphic Reactions at Elevated Temperatures and Pressures: An Appraisal of Available Experimental Data". W Metamorphic Reactions, 27–79. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5066-1_2.
Pełny tekst źródłaSmith, B. K. "The Influence of Defect Crystallography on Some Properties of Orthosilicates". W Metamorphic Reactions, 98–117. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5066-1_4.
Pełny tekst źródłaTracy, R. J., i E. L. McLellan. "A Natural Example of the Kinetic Controls of Compositional and Textural Equilibration". W Metamorphic Reactions, 118–37. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5066-1_5.
Pełny tekst źródłaBrodie, K. H., i E. H. Rutter. "On the Relationship between Deformation and Metamorphism, with Special Reference to the Behavior of Basic Rocks". W Metamorphic Reactions, 138–79. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5066-1_6.
Pełny tekst źródłaKnipe, R. J., i R. P. Wintsch. "Heterogeneous Deformation, Foliation Development, and Metamorphic Processes in a Polyphase Mylonite". W Metamorphic Reactions, 180–210. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4612-5066-1_7.
Pełny tekst źródłaStreszczenia konferencji na temat "Metamorphic reaction"
Hoisch, Thomas D., Suzanne D. Craddock i Eric D. Kelly. "EXCESS GARNET GROWTH IN METAMORPHIC ROCKS DRIVEN BY REACTION AFFINITY ASSOCIATED WITH OVERSTEPPED REACTIONS". W GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300296.
Pełny tekst źródłaKonrad-Schmolke, Matthias. "How Well do We Know Reaction Pathways in Metamorphic Rocks?" W Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1353.
Pełny tekst źródłaFoster, C. T. "EQUILIBRIUM....OR NOT? CLUES FROM REACTION MECHANISMS IN METAMORPHIC ROCKS". W GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-282558.
Pełny tekst źródłaBanerjee, Meenakshi, Upama Dutta, Vedanta Adak i Raima Ghosh. "PARAMETERS CHARACTERIZING INFLUENCE ON PRODUCT COMPOSITION IN METAMORPHIC REACTION: AN APPROACH USING CHEMICAL POTENTIAL DIAGRAM". W GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-383835.
Pełny tekst źródłaFranke, Mees, Bastian Joachim-Mrosko, Roland Stalder i Burkhard Schmidt. "Metamorphic reaction kinetics at "dry" and "wet" conditions in the binary MgO-SiO2 system". W Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10913.
Pełny tekst źródłavan der Wijk, Volkert, Ketao Zhang i Jian S. Dai. "Force Balance of a Spatial Metamorphic 6R Closed-Chain Linkage With Specific Kinematic Conditions". W ASME 2016 International Design Engineering Technical Conferences and Computers and Information in Engineering Conference. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/detc2016-60068.
Pełny tekst źródłaBarré, G., E. Thomassot, P. Cartigny, R. Michels, L. Truche, P. Strzerzynski, S. Guillot, C. Lorgeoux i N. Assayag. "How Multiple Sulfur Isotopes (δ33S, δ34S, δ36S) Help Unravel the Context of Thermochemical Sulfate Reaction during Metamorphic Events: Application to Subducted Evaporites from the French Alps". W First EAGE/IFPEN Conference on Sulfur Risk Management in Exploration and Production. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201802767.
Pełny tekst źródłaHelman, Daniel. "Microtectonics and Electricity: Diffusion Rate Variabilities in Metamorphic Reactions." W Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.8554.
Pełny tekst źródłaFagan, T. J., i Y. Endo. "FROM METAMORPHISM IN NEW ENGLAND TO RED-OX REACTIONS IN THE SOLAR NEBULA: A LONG AND WINDING ROAD THROUGH REACTION SPACE". W 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310833.
Pełny tekst źródłaBarbato, Allison Kay, Barbara L. Dutrow i Darrell J. Henry. "CATHODOLUMINESCENCE AND TRACE ELEMENT CHEMISTRY OF SILLIMANITE: EVIDENCE FOR MULTIPLE METAMORPHIC REACTIONS". W GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-299153.
Pełny tekst źródłaRaporty organizacyjne na temat "Metamorphic reaction"
Papike, J. J., i C. K. Shearer. Cores from the Salton Sea scientific drilling program: Metamorphic reaction progress as a function of chemical and thermal environment: Final report. Office of Scientific and Technical Information (OSTI), maj 1987. http://dx.doi.org/10.2172/6562428.
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