Institut für Geo- und Umweltnaturwissenschaften

Mineralogie - Petrologie 

Albertstraße 23b   

79104 Freiburg i. Br.       

Tel.: +49 (0)761 -203-6396  





  • Hong T., Dolejš D., Zhai M.-G., Laurent O., Xu X.-W., Gao J., Schlöglová K.D., Wang Y.-J. (2021): Multiple tectonic-magmatic Mo-enrichment events in Yuleken porphyry Cu-Mo deposit, NW China and its implications for the formation of giant porphyry Mo deposit. Ore Geology Reviews, 104401. DOI
  • Huang R., Boffa Ballaran T., McCammon C.A., Miyajima N., Dolejš D., Frost D. (2021): The composition and redox state of bridgmanite in the lower mantle as a function of oxygen fugacity. Geochimica et Cosmochimica Acta, 303, 110-136. DOI
  • Peterková T., Dolejš D. (2019): Magmatic-hydrothermal transition of Mo-W-mineralized granite-pegmatite-greisen system recorded by trace elements in quartz: Krupka district, Eastern Krušné hory/Erzgebirge. Chemical Geology, 523, 179-202. DOI
  • Dolejš D., Zajacz Z. (2018): Halogens in silicic magmas and their hydrothermal systems. In: Harlov D.E., Aranovich L. (eds.): The role of halogens in terrestrial and extraterrestrial geochemical processes. Springer, Cham, 431-543. DOI
  • Guo H., Audétat A., Dolejš D. (2018): Solubility of gold in oxidized, sulfur-bearing fluids at 500-850 'C and 200-230 MPa: a synthetic fluid inclusion study. - Geochimica et Cosmochimica Acta, 222, 655-670. DOI
  • Chust T., Steinle-Neumann G., Dolejš D., Schuberth B.S.A., Bunge H.-P. (2017): MMA-EoS - a computational framework for mineralogical thermodynamics. - Journal of Geophysical Research: Solid Earth, 122, 9881-9920. DOI
  • Schlöglova K., Wälle M., Heinrich C.A., Dolejš D. (2017): Copper, gold and bismuth behavior in magmatic-hydrothermal systems: fluid-inclusion LA-ICP-MS study. - Proceedings 14th SGA Biennial Meeting, 1-4, 95-98.
  • Dolejš D., Špillar V. (2017): Von Magma zum Gestein: wie bilden sich die Kristalle? - Freiburger Universitätsblätter 216, 21-36.
  • Novella D., Dolejš D., Myhill R., Pamato M. G., Manthilake G., Frost D. J. (2017): Melting phase relations in the systems Mg2SiO4-H2O and MgSiO3-H2O and the formation of hydrous melts in the upper mantle. - Geochimica et Cosmochimica Acta, 204, 68-82. DOI
  • Dolejš D. (2016): Ions surprise in Earth's deep fluids. Nature, 539, 362-364. DOI
  • Dolejš D., Bendl J., Štemprok M. (2016): Rb-Sr isotopic composition of granites in the Western Krušné hory/Erzgebirge pluton, Central Europe: Record of variations in source lithologies, mafic magma input and postmagmatic hydrothermal events. – Mineralogy and Petrology, 110, 601-622. DOI
  • Babuška V., Růžek V., Dolejš D. (2016): Origin of earthquake swarms in the western Bohemian Massif: is the mantle CO2 degassing, followed by the Cheb Basin subsidence, an essential driving force? - Tectonophysics, 668-669, 42-51. DOI
  • Špillar V., Dolejš D. (2015): Melt extraction from crystal mushes: Numerical model of texture evolution and calibration of crystallinity-ordering relationships. - Lithos 239, 19-32.DOI
  • Chemia Z., Dolejš D., Steinle-Neumann G. (2015): Thermal effects of variable material properties and metamorphic reactions in a three-component subducting slab. - Journal of Geophysical Research, Solid Earth 120, 6823-6845. DOI
  • Dolejš D. (2015): Quantitative characterization of hydrothermal systems and reconstruction of fluid fluxes: the significance of advection, disequilibrium, and dispersion. - Proceedings 13th SGA Biennial Meeting, vol. 2, 445-448.PDF
  • Jandová T., Dolejš D., Trubač J. (2015): Internal evolution and disequilibrium crystallization of a highly fractionated, Sn-Nb-Ta-bearing granite-pegmatite system: a case study from the Říčany pluton, Czech Republic. - Proceedings 13th SGA Biennial Meeting, vol. 2, 769-772.PDF
  • Špillar V., Dolejš D. (2015): Heterogeneous nucleation as the predominant mode of crystallization in natural magmas: Numerical model and implications for crystal-melt interaction. - Contributions to Mineralogy and Petrology 169, 4, 16 p. DOI
  • Honig S., Čopjaková R., Škoda R., Novák M., Dolejš D., Leichmann J., Vašinová Galiová M. (2014): Garnet as a major carrier of the Y and REE in the granitic rocks: An example from the layered anorogenic granite in the Brno batholith, Czech Republic. - American Mineralogist 99, 1922-1941. DOI
  • Špillar V., Dolejš D. (2014): Kinetic model of nucleation and growth in silicate melts: Implications for igneous textures and their quantitative description. - Geochimica et Cosmochimica Acta 131, 164-183. DOI
  • Sun W., Audétat A., Dolejš D. (2014): Solubility of molybdenite in hydrous granitic melts at 800 'C, 100-200 MPa. - Geochimica et Cosmochimica Acta 131, 393-401. DOI
  • Štemprok M., Dolejš D., Holub F. V. (2014): Late Variscan calc-alkaline lamprophyres in the Krupka ore district, Eastern Krušné hory/Erzgebirge: their relationship to Sn-W mineralization. - Journal of Geosciences 59, 41-68. DOI
  • Heřmanská M., Dolejš D. (2013): Reactive fluid flow and integrated fluxes recorded by tin-bearing greisens, Krušné hory (Erzgebirge) Mts., central Europe. - Proceedings 12th SGA Biennial Meeting, vol. 3, 1267-1270.
  • Bubal J., Dolejš D. (2013): Magnetite chemistry in skarns of the Bohemian Massif: evaluating competing effects of protolith inheritance, crystal chemistry, fluid composition and pressure-temperature conditions. - Proceedings 12th SGA Biennial Meeting, vol. 1, 264-267.
  • Dolejš D. (2013): Thermodynamics of aqueous species at high temperatures and pressures: equations of state and transport theory. - Reviews in Mineralogy and Geochemistry 76, 35-79. DOI
  • Bernini D., Audétat A., Dolejš D., Keppler H. (2013): Zircon solubility in aqueous fluids at high temperatures and pressures. - Geochimica et Cosmochimica Acta 119, 178-187. DOI
  • Špillar V., Dolejš D. (2013): Calculation of time-dependent nucleation and growth rates from quantitative textural data: Inversion of crystal size distribution. - Journal of Petrology 54, 913-931. DOI
  • Bernini D., Wiedenbeck M., Dolejš D., Keppler H. (2013): Partitioning of halogens between mantle minerals and aqueous fluids: Implications for the fluid flow regime in the subduction zones. - Contributions to Mineralogy and Petrology 165, 117-128. DOI
  • Zhang L., Audétat A., Dolejš D. (2012): Solubility of molybdenite (MoS2) in aqueous fluids at 600-800 'C, 200 MPa: A synthetic fluid inclusion study. - Geochimica et Cosmochimica Acta 77, 175-185. DOI
  • Nahodilová R., Faryad S. W., Dolejš D., Tropper P., Konzett J. (2011): High pressure partial melting and melt loss in felsic granulites in the Kutná Hora complex, Bohemian Massif (Czech Republic). - Lithos 125, 641-658. DOI
  • Vondrovic L., Trubač J., Dobeš P., Dolejš D. (2011): Origin of wolframite mineralization at Jeřmanice (central Europe): evidence from mineral chemistry, fluid inclusions and stable isotopes. - Proceedings 11th SGA Biennial Meeting, 225-227.
  • Audétat A., Dolejš D., Lowenstern J. B. (2011): Molybdenite saturation in silicic magmas: Occurrence and petrological implications. - Journal of Petrology 52, 891-904. DOI
  • Dolejš D., Manning C. E. (2010): Thermodynamic model for mineral solubility in aqueous fluids: Theory, calibration and application to model fluid-flow systems. - Geofluids 10, 20-40. DOI
  • Štemprok M., Dolejš D. (2010): Fluid focusing, mass transfer and origin of fracture-controlled greisens in the Western Krušné hory granite pluton, Central Europe. - Zeitschrift fur geologische Wissenschaften 38, 207-234.
  • Kalo H., Moller M. W., Ziadeh M., Dolejš D., Breu J. (2010): Large scale melt synthesis in an open crucible of Na-fluorohectorite with superb charge homogeneity and particle size. - Applied Clay Science 48, 39-45. DOI
  • Faryad S. W., Nahodilová R., Dolejš D. (2010): Incipient eclogite facies metamorphism in the Moldanubian granulites revealed by mineral inclusions in garnet. - Lithos 114, 54-69. DOI
  • Faryad S. W., Dolejš D., Machek M. (2009): Garnet exsolution in pyroxene from clinopyroxenites in the Moldanubian zone: Constraining the early pre-convergence of ultramafic rocks in the Variscan orogen. - Journal of Metamorphic Geology 27, 655-671. DOI
  • Arefin M. L., Raether F., Dolejš D., Klimera A. (2009): Phase formation during liquid phase sintering of ZnO ceramics. - Ceramics International 35, 3313-3320. DOI
  • Štemprok M., Seifert T., Holub F. V., Chlupáčová M., Dolejš D., Novák J. K., Pivec E., Lang M. (2008): Petrology and geochemistry of Variscan dykes from Jáchymov (Joachimsthal) ore district, Czech Republic. - Journal of Geosciences 53, 65-104. DOI
  • Rouquette J., Dolejš D., Kantor I. Yu., McCammon C. A., Frost D. J., Prakapenka V. B., Dubrovinsky L. S. (2008): Iron-carbon interactions at high pressure. - Applied Physics Letters 92, 121912. DOI
  • Dolejš D., Wagner T. (2008): Thermodynamic modeling of non-ideal mineral-fluid equilibria in the system Si-Al-Fe-Mg-Ca-Na-K-H-O-Cl at elevated temperatures and pressures: Implications for hydrothermal mass in granitic rocks. - Geochimica et Cosmochimica Acta 72, 526-553. DOI
  • Štemprok M., Dolejš D., Muller A., Seltmann R. (2008): Textural evidence of magma decompression, devolatilization and disequilibrium quenching: An example from the Western Krušné hory/Erzgebirge granite pluton. - Contributions to Mineralogy and Petrology 155, 93-109. DOI
  • Piazzoni A. S., Steinle-Neumann G., Bunge H.-P., Dolejš D. (2007): A mineralogical model for the density and elasticity of the Earth's mantle. - Geochemistry, Geophysics, Geosystems 8, Q11010. DOI
  • Frost D. J., Dolejš D. (2007): Experimental determination of the effect of H2O on the 410-km seismic discontinuity. - Earth and Planetary Science Letters 256, 182-195. DOI
  • Dolejš D., Baker D. R. (2007): Liquidus equilibria in the system K2O-Na2O-Al2O3-SiO2-F2O-1-H2O to 100 MPa: II. Differentiation paths of fluorosilicic magmas in hydrous systems. - Journal of Petrology 48, 807-828. DOI
  • Dolejš D., Baker D. R. (2007): Liquidus equilibria in the system K2O-Na2O-Al2O3-SiO2-F2O-1-H2O to 100 MPa: I. Silicate-fluoride liquid immiscibility in anhydrous systems. - Journal of Petrology 48, 785-806. DOI
  • Dolejš D., Baker D. R. (2006): Fluorite solubility in hydrous haplogranitic melts at 100 MPa. - Chemical Geology 225, 40-60. DOI
  • Dolejš D., Baker D. R. (2006): Phase transitions and volumetric properties of cryolite, Na3AlF6: Differential thermal analysis to 100 MPa. - American Mineralogist 91, 97-103. DOI
  • Dolejš D., Baker D. R. (2005): Thermodynamic modeling of melts in the system Na2O-NaAlO2-SiO2-F2O-1. - Geochimica et Cosmochimica Acta 69, 5537-5556. DOI
  • Dolejš D. (2005): Evidence for fluoride melts in Earth's mantle formed by liquid immiscibility: comment. - Geology 33, e76.
  • Janoušek V., Finger F., Roberts M., Frýda J., Pin C., Dolejš D. (2004): Deciphering the petrogeneis of deeply buried granites: Whole-rock geochemical constraints on the origin of largely undepleted felsic granulites from the Moldanubian Zone of the Bohemian Massif. - Transactions of the Royal Society of Edinburgh Earth Sciences 95, 141-159.
  • Schatz O., Dolejš D., Stix J., Williams-Jones A. E., Layne G. D. (2004): Partitioning of boron among melt, brine and vapor in the system haplogranite-H2O-NaCl at 800 C and 100 MPa. - Chemical Geology 210, 135-147. DOI
  • Audétat A., Pettke T., Dolejš D. (2004): Magmatic anhydrite and calcite in the ore-forming quartz-monzodiorite magma at Santa Rita, New Mexico (USA): Genetic constraints on porphyry-Cu mineralization. - Lithos 72, 147-161. DOI
  • Dolejš D., Baker D. R. (2004): Thermodynamic analysis of the system Na2O-K2O-CaO-Al2O3-SiO2-H2O-F2O-1: Stability of fluorine-bearing minerals in felsic igneous suites. - Contributions to Mineralogy and Petrology 146, 762-778. DOI
  • Dolejš D., Štemprok M. (2001): Magmatic and hydrothermal evolution of Li-F granites: Cínovec and Krásno intrusions, Krušné hory batholith, Czech Republic. - Bull. Czech Geol. Surv. 76, 77-99.
  • Hrouda F., Táborská Š., Schulmann K., Ježek J., Dolejš D. (1999): Magnetic fabric and rheology of co-mingled magmas in the Nasavrky Plutonic Complex (E Bohemia): Implications for intrusive strain regime and emplacement mechanism. - Tectonophysics 307, 93-111. DOI
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