Wordmark GFZ Potsdam

Publications

 
(Co) Author: Förster, H.-J.
(since 1994) [ All ]



































  • Förster, H.-J.; Rhede, D. (2006): The Be-Ta-rich granite of Seiffen (eastern Erzgebirge, Germany): accessory-mineral chemistry, composition, and age of late-Variscan Li-F granite of A-type affinity. Neues Jahrbuch für Mineralogie, Abhandlungen, 182, 3, 307-321.







  • Förster, H.-J. (2005): Mineralogy of the Niederschlema–Alberoda U–Se-polymetallic deposit, Erzgebirge, Germany. IV. The continuous clausthalite–galena solid-solution series. Neues Jahrbuch für Mineralogie Abhandlungen, 181, 2, 125-134.








  • Förster, H.-J. (2004): Mineralogy of the Niederschlema–Alberoda U–Se-polymetallic deposit, Erzgebirge, Germany. II. Hessite, Ag2Te, and native Te(?), the first tellurium minerals. Neues Jahrbuch für Mineralogie Abhandlungen, 180, 2, 101-113.

  • Förster, H.-J.; Rhede, D. (2004): Mineralogy of the Niederschlema - Alberoda U-Se-polymetallic deposit, Erzgebirge, Germany. III. First indication for complete miscibility between tennantite and giraudite. The Canadian Mineralogist, 42, 6, 1719-1732.

  • Förster, H.-J.; Rhede, D.; Tischendorf, G. (2004): Mineralogy of the Niederschlema - Alberoda U-Se-polymetallic deposit, Erzgebirge, Germany. I. Jolliffeite, NiAsSe, the rare Se analogue of gersdorffite. Canadian Mineralogist, 42, 3, 841-849.






  • Harlov, D. E.; Förster, H.-J. (2003): Fluid-induced nucleation of (Y+REE)-phosphate minerals within apatite: Nature and experiment. Part II. Fluorapatite. American Mineralogist, 88, 8-9, 1209-1229.

  • Harlov, D. E.; Förster, H.-J.; Schmidt, C. (2003): High P-T experimental metasomatism of a fluorapatite with significant britholite and fluorellestadite components: implications for LREE mobility during granulite-facies metamorphism. Mineralogical Magazine, 67, 1, 61-72.

  • Thomas, R.; Förster, H.-J.; Heinrich, W. (2003): The behaviour of boron in peraluminous granite-pegmatite systems and associated hydrothermal solutions: a melt and fluid inclusion study. Contributions to Mineralogy and Petrology, 144, 4, 457-472.




  • Harlov, D. E.; Förster, H.-J. (2002): High grade fluid metasomatism on both a local and regional scale: the Seward Penninsula, Alaska and the Ivrea-Verbano Zone, Northern Italy. Part II: Phosphate mineral chemistry. Journal of Petrology, 43, 5, 801-824.

  • Harlov, D. E.; Förster, H.-J. (2002): High-grade fluid metasomatism on both a local and regional scale: the Seward Penninsula, Alaska and the Ivrea-Verbano Zone, Northern Italy. Part I: Petrography and silicate mineral chemistry. Journal of Petrology, 43, 5, 769-799.




  • Förster, H.-J. (2001): Synchysite-(Y) - synchisite-(Ce) solid solutions from Markersbach, Erzgebirge, REE and Th mobility during high-T alteration of highly fractionated aluminous A-type granites.. Mineralogy and Petrology, 72, 4, 259-280.

  • Förster, H.-J.; Tischendorf, G. (2001): Se-rich tennantite and constraints on p-T-X conditions of selenide mineral formation in the Schlema-Alberoda uranium ore district (western Erzgebirge, Germany).. Neues Jahrbuch für Mineralogie - Abhandlungen, 176, 2, 109-126.




  • Förster, A.; Förster, H.-J. (2000): Crustal composition and mantle heat flow: implications from surface heat flow and radiogenic heat production in the Variscan Erzgebirge (Germany). Journal of Geophysical Research, 105, B12, 27917-27938.

  • Förster, H.-J. (2000): Cerite-(Ce) and thorian synchysite-(Ce) from Niederbobritzsch granite (Erzgebirge, Germany): implications for the differential mobility of Th and the LREE during alteration. Canadian Mineralogist, 38, 1, 67-79.

  • Förster, H.-J.; Davis, J. D. (2000): Determination of geochemical affinities of granitic rocks from the Aue-Schwarzenberg Zone (Erzgebirge, Germany) by multivariate statistics. Neues Jahrbuch für Mineralogie, Monatshefte, 12, 529-542.




  • Förster, H.-J. (1999): The chemical composition of uraninite in Variscan granites of the Erzgebirge, Germany. Mineralogical Magazine, 63, No. 417, 239-252.


  • Förster, H.-J.; Harlov, D. E. (1999): Monazite-(Ce) - huttonite solid solutions in granulite-facies metabasites from the Ivrea-Verbano Zone, Italy. Mineralogical Magazine, 63, No. 419, 587-594.




  • Förster, H.-J. (1998): The chemical composition of REE-Y-Th-U-rich accessory minerals from peraluminous granites of the Erzgebirge-Fichtelgebirge region, Germany. Part I: The monazite-(Ce) - brabantite solid solution series. American Mineralogist, 83, No. 3-4, 259-272.

  • Förster, H.-J. (1998): The chemical composition of REE-Y-Th-U-rich accessory minerals from peraluminous of the Erzgebirge-Fichtelgebirge region, Germany. Part II: Xenotime. American Mineralogist, 83, No. 11-12, 1302-1315.













  • Förster, H.-J. (2010): The late-Variscan granites of the Aue-Schwarzenberg Zone (western Erzgebirge, Germany): Composition of accessory minerals and mineralogical mass balance of the lanthanides and actinides. Zeitschrift für geologische Wissenschaften, 38, 2-3, 125-144.


  • Trumbull, R. B.; Förster, H.-J.; Rhede, D. (2010): REE-Y-Th-U-bearing accessory minerals and their contribution to the lanthanide and actinide trace-element budget in an anorogenic granite from the Erongo Complex, NW Namibia. Zeitschrift für geologische Wissenschaften, 38, 2-3, 145-166.




  • Förster, H.-J. (2000): On the origin of the Kösseine granites and their enclaves (Fichtelgebirge, Germany): Implications from the composition and age of REE-bearing accessory minerals. Münchner Geologische Hefte, A28, 35-51.

  • Tischendorf, G.; Förster, H.-J.; Gottesmann, B. (2000): Tri- und dioktaedrische Glimmer in Granitoiden aus dem Osten Deutschlands - Historie ihrer Untersuchung und neue Forschungsergebnisse. Zeitschrift für Geologische Wissenschaften, 25, 5-6, 427-442.



  • Tischendorf, G.; Förster, H.-J.; Gottesmann, B. (1999): Tri- und dioktaedrische Glimmer in Granitoiden aus dem Osten Deutschlands - Historie ihrer Untersuchung und neue Forschungsergebnisse. Zeitschrift für Geologische Wissenschaften, 27, 5-6, 427-442.




  • Förster, H.-J.; Romer, R. L. (2010): Carboniferous Magmatism. - In: Linnemann, U.; Romer, R. L. (Eds.), Pre-Mesozoic Geology of Saxo-Thuringia: From the Cadomian Active Margin to the Variscan Orogen, Schweizerbart, 287-308.


  • Förster, H.-J.; Tischendorf, G. (2008): Granitoide Intrusivformationen, Kap. 3.4.2.1 Erzgebirge–Vogtland. - In: Pälchen, W.; Walter, H. (Eds.), Geologie von Sachsen, Schweizerbart, 260-274.

  • Förster, H.-J.; Tischendorf, G. (2008): Kap. 3.4.4 Zur Metallogenie des spätvariszischen Magmatismus und des Molassestockwerks. - In: Pälchen, W.; Walter, H. (Eds.), Geologie von Sachsen, Schweizerbart, 293-296.







  • Förster, H.-J. (1995): Types of uranium and fluorite-barite deposits. - In: Breiter, K.; Seltmann, R. (Eds.), Exkursion Guide: Ore Mineralization of the Krusne hory Mts. (Erzgebirge), 3rd Biennial SGA Meet. "Mineral Deposits: From the Origin to their Environmental Impact", Czech Geological Survey, 41-45.





  • Tischendorf, G.; Förster, H.-J. (1994): Hercynian granite magmatism and related metallogenesis in the Erzgebirge: A status report. - In: von Gehlen, K.; Klemm, D. D. (Eds.), Mineral Deposits of the Ergebirge/Kru_né hory (Germany/Czech Republic). - Monograph Series on Minera, 5-23.


  • 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.


  • Davis, J. C.; Förster, H.-J. (1998): Canonical analysis of composition of granite plutons from the German Erzgebirge: Implications for granite classification and petrogenesis. 4th Ann. Conf. Int. Assoc. Mathematical Geology, 410-414.



  • Harlov, D. E.; Förster, H.-J. (1998): Monazite-(Ce)-huttonite solid solutions in granulite-facies metabasites from the Ivrea-Verbano Zone, N. Italy: The role of phosphate minerals in high-grade fluid flow. Geological Soc. of London, Meet. of the Metamorphic Studies group "Behaviour of accessory phases, 8 (L).



  • Förster, H.-J. (1997): Xenotime - its compositional diversity and bearing on the HREE evolution in peraluminous granites. 7th Goldschmidt Conference, 73-74.








  • Förster, H.-J.; Rhede, D. (1995): Composition of Monazite and Xenotime from the Fichtelgebirgs granites - An electron microprobe study. MINERALOGIE 95, Gem. Tagung SFMC, DMG, ÖMG.

  • Förster, H.-J.; Rhede, D. (1995): Extreme compositional variability in granitic monazites. 3rd Hutton Symp. on the Origin of Granites and Related Rocks, 54-55.







  • Förster, H.-J. (1994): Accessory mineral behaviour during differentiation of composite granite plutons in the Erzgebirge. IMA 16th General Meet., p. 123 (L).

  • Förster, H.-J.; Tischendorf, G. (1994): Evolution of the Hercynian granite magmatism in the Erzgebirge metallogenic province. 4th Annual Goldschmidt Conference (Edinburgh 1994), 284-285.




  • (2012): Granites of the Erzgebirge : relation of magmatism to the metamorphic and tectonic evolution of the Variscan Orogen ; guidebook to Eurogranites 2012 fieldtrip October 7 to October 13, 2012. Scientific Technical Report ; 12/15, Deutsches GeoForschungsZentrum GFZ, 122.



  • Förster, H.-J.; Förster, A. (2010): Abschlussbericht zum Ingenieurvertrag 'Exploration von thermischen Gesteinsparametern und Temperaturfeldern im Bearbeitungsgebiet Annaberg-Buchholz'. Geoforschungszentrum, 40 S..

  • Förster, H.-J.; Förster, A. (2010): Thermische Gesteinsparameter und Temperaturfeld. Abschlußbericht zum Forschungs- und Entwicklungsvertrag, Deutsches GeoForschungsZentrum, 1-80.








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