Wordmark GFZ Potsdam

Publications

 
(Co) Author: Förster, H.-J.
(since 1999) [ All ]

  • Fuchs, S.; Schütz, F.; Förster, A.; Förster, H.-J. (2012): Evaluation of common mixing models for calculating bulk thermal conductivity of sedimentary rocks: correction charts and new conversion equations. GeoEn International Conference - GeoEnergy (Potsdam, Germany 2012), 73.

  • Förster, A.; Förster, H.-J. (2012): The thermal regime of the Arabian Plate. Abstract Volume, International Conference on the Geology of the Arabian Plate and the Oman Mountains (ICGAPOM) (Muscat, Oman 2012), 81.

  • Schütz, F.; Förster, A.; Förster, H.-J.; Weber, M. (2012): Heat flow and lithospheric thermal structure of the western Arabian Shield. Abstract Volume, International Conference on the Geology of the Arabian Plate and the Oman Mountains (ICGAPOM) (Muscat, Oman 2012), 223.




  • Förster, A.; Förster, H.-J. (2010): Exploring for deep heat in stable igneous provinces. Technical Program Abstracts, Symposium on 'Kansas Geophysics in the 21st Century' (Wichita, Kansas 2010), 12.





  • Förster, A.; Förster, H.-J. (2009): Surface heat flow of the Arabian Plate and related temperature regimes.. Lithosphere dynamics and sedimentary basins: The Arabian plate and analogues ; Abstracts with Programme, 5th workshop of the ILP-Task Force on Sedimentary Basins (Abu Dhabi, United Arab Emirates 2009), 46-48.








  • Förster, A.; Förster, H.-J. (2006): Exploring for radiogenic heat: A case study from the Saxothuringian zone of Germany. Actes/Abstracts of the Engine Workshop 1 'Defining, Exploring, Imaging and Assessing Reservoirs for Potential Heat Exchange', ENGINE Workshop 1 - Defining, Exploring, Imaging and Assessing Reservoirs for Potential Heat Exchange (Potsdam, Germany 2006), 18.








  • Harlov, D. E.; Wirth, R.; Förster, H.-J. (2004): Dissolution-reprecipitation in fluorapatite: fluid infiltration and formation of metasomatic monazite. 14th Annual Goldschmidt Conference (Copenhagen, Denmark 2004), A181.

  • Thomas, R.; Förster, H.-J.; Rickers, K.; Webster, J. D. (2004): Formation of extreme F-rich hydrous melt fractions and hydrothermal fluids during differentiation of highly evolved tin-granite magmas: a complex melt/fluid inclusion study. 14th Annual Goldschmidt Conference (Copenhagen, Denmark 2004).



  • Förster, A.; Förster, H.-J.; Stromeyer, D. (2003): An internally consistent present-day thermo-petrological model of the Erzgebirge crust. Geology Without Frontiers: Magmatic and Metamorphic Evolution of the Central European Variscides (Blansko 2003), 49-50.


  • Harlov, D. E.; Förster, H.-J. (2003): Nucleation and growth of monazite and xenotime in fluorapatite: the role of P-T, fluids, and crystal chemistry. EGS-AGU-EUG Joint Assembly (Nice 2003), 03669.


  • Harlov, D. E.; Wirth, R.; Förster, H.-J. (2003): Physical properties of the interface between a mineral inclusion and the host mineral: monazite inclusions in fluorapatite. AGU 2003 Fall Meeting (San Francisco 2003).


  • Harlov, D. E.; Förster, H.-J. (2002): Experimentally induced nucleation of monazite from fluorapatite: the importance of fluid composition. 9th International Symposium on Experimental Mineralogy, Petrology and Geochemistry (Zürich 2002), 43.

  • Harlov, D. E.; Förster, H.-J. (2002): Formation of monazite from metasomatised fluorapatite: experimental evidence for the importance of fluid chemistry. 18th General Meeting of the International Mineralogical Association (Edinburgh 2002), 236-237.

  • Thomas, R.; Förster, H.-J.; Heinrich, W. (2002): The behavior of boron in peraluminous granite-pegmatite systems and associated hydrothermal solutions: A melt and fluid inclusion study. 8th Biennial Pan-American Conference on Research on Fluid Inclusions (PACROFI) (Halifax 2002).



  • Förster, A.; Förster, H.-J. (2001): Inferring crustal structure and composition from heat-flow pattern: Experience from the Variscan Erzgebirge, Germany. 11th Meet. Europ. Union Geosciences (Strasbourg France 2001), 640.

  • Förster, H.-J. (2001): The radioactive accessory-mineral assemblage of the Podlesi granite-pegmatite system, western Krusne, Czech Republic: Implications to intrusion age and magmatic/hydro-thermal fluid-rock interaction. In: K. Breiter (ed.). Int. Workshop "Phosphorus- and fluorine-rich fractionated granites", 14-15.

  • Förster, H.-J. (2001): Thorite-zircon-coffinite-xenotime solid solutions: Composition and origin.. 11th Meet. of the EUG, 676.

  • Förster, H.-J.; Förster, A. (2001): Processes controlling the distribution of heat-producing elements in the Earth's upper crust. 5th Int. Meet. "Heat Flow and the Structure of the Lithosphere" (Kostelec nad Cernymi Lesy Czech Republic 2001, 17.

  • Harlov, D. E.; Förster, H.-J. (2001): Dehydration of the mafic lower crust from amphibolite to granulite facies and the role of high grade, low water activity fluids: petrographic and mineralogical evidence. Tectonics and Magma 2001, IGCP-Project 373, 41-42.

  • Harlov, D. E.; Förster, H.-J. (2001): Fluid induced nucleations of monazite and/or xenotime in apatite. 79. Jahrestagung der Deutschen Mineralogischen Gesellschaft (Potsdam 2001), 73.



  • Harlov, D. E.; Förster, H.-J. (2000): Experimental nucleation of co-existing monazite and xenotime grains in chlorapatite. 10th Annual Goldschmidt Conference (Oxford 2000), 486.

  • Harlov, D. E.; Förster, H.-J. (2000): Experimental nucleation of co-existing monazite and xenotime grains in chlorapatite using H2O-rich fluids under high pressure and temperature. 8th International Symposium on Experimental Mineralogy, Petrology and Geochemistry (Bergamo 2000), 46.


  • Förster, A.; Förster, H.-J. (1999): Heat Flow and lithospheric structure in the Variscan of Europe: The potential and problems of Q-A plots. XXIV General Assembly Europ. Geophys. Soc., 75 (P).

  • Förster, H.-J. (1999): Petrological constraints on the geodynamic evolution of the Variscan Erzgebirge, Germany. XXIV General Assembl. of the Europ. Geophys. Soc., 73.

  • Harlov, D. E.; Förster, H.-J. (1999): Monazite-group minerals in granulite-facies metabasites from the Ivrea-Verbano Zone, N. Italy: implications for high grade fluid flow. EUG 10, 712 (L).

  • Harlov, D. E.; Förster, H.-J. (1999): Phosphate mineral chemistry and high grade fluid metasomatism on both a local and regional scale: the Seward Penninsula, Alaska and the Ivrea-Verbano Zone, Northern Italy. Martine Lagache High Grade Fluid Workshop, 107-108.

  • Romer, R. L.; Förster, H.-J.; Breitkreuz, C. (1999): Compositional, isotopic and mineralogical constraints on the inhomogeneous nature of rhyolites from the late Carboniferous Halle Volcanic Complex (Germany). 89. Jtg. der Geol. Vereinig., 170.





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