Wordmark GFZ Potsdam

Publications

 
(Co) Author: Harlov, D.









  • Harlov, D. E. (2011): Formation of monazite and xenotime inclusions in fluorapatite megacrysts, Gloserheia Granite Pegmatite, Froland, Bamble Sector, southern Norway. Mineralogy and Petrology, 102, 1-4, 77-86.











  • Harlov, D. E. (2010): Th and U incorporation into xenotime during partial alteration by alkali-bearing fluids. Geochimica et Cosmochimica Acta, 74, 12, Suppl. 1, A382.








  • Hansen, E. C.; Harlov, D. E. (2009): Orthophosphate and biotite chemistry from orthopyroxene-bearing migmatites from California and South India: The role of a fluid-phase in the evolution of granulite-facies migmatites. Mineralogy and Petrology, 95, 3-4, 201-217.



  • Tropper, P.; Manning, C. E.; Harlov, D. (2009): Solubility of CePO4 and YPO4 in H2O, H2O-NaCl and H2O-NaF at 800 degrees C and 1 GPa: Implications for REE transport during high-grade metamorphism. Geochimica et Cosmochimica Acta, 73, 13, Suppl. 1, A1348.











  • Harlov, D. E. (2007): Metasomatically induced alteration and re-equilibration of orthophosphate and silicate minerals: Textures, fluids, and mass transfer. Geochimica et Cosmochimica Acta, 71, 15, Suppl. 1, A381.























  • 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.





  • 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.


  • Harlov, D. E.; Melzer, S. (2002): Experimental Partitioning of Rb and K between Phlogopite and a Supercritical (K,Rb)Cl Brine: Implications for the Role of Supercritical KCl Brines in the Depletion of Rb in Phlogopite and the Stability of Phlogopite During Charnockite Genesis. Lithos, 64, 15-28.

  • Harlov, D. E.; Milke, R. (2002): Stability of corundum + quartz relative to kyanite and sillimanite at high temperature and pressure. American Mineralogist, 87, 424-432.










  • Harlov, D. E. (2000): Apparent pyrrhotite-chalcopyrite solid solutions in charnockites: the Shevaroy Hills Massif, Tamil Nadu, S India and the Bamble Sector, SE Norway. Mineralogical Magazine, 64, 5, 853-865.

  • Harlov, D. E. (2000): Pressure-temperature estimation in orthopyroxene-garnet bearing granulite facies rocks, Bamble Sector, Norway. Mineralogy and Petrology, 69, 1-2, 11-33.

  • Harlov, D. E. (2000): Titaniferous magnetite-ilmenite thermometry / titaniferous magnetite-ilmenite-orthopyroxene-quartz oxygen barometry in orthopyroxene-bearing granulite facies gneisses, Bamble Sector, SE Norway: implications for the role of high grade CO2-rich fluids durin. Contributions to Mineralogy and Petrology, 139, 2, 180-197.

  • Harlov, D. E.; Wirth, R. (2000): K-feldspar-quartz phase and K-feldspar-plagioclase phase boundary interactions in garnet-orthopyroxene gneisses from Val Strona di Omegna, Ivrea-Verbano Zone, Northern Italy: a case for high grade emplacement under relatively dry conditions. Contributions to Mineralogy and Petrology, 140, 2, 148-162.



  • 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.

  • Harlov, D. E. (1999): Ag-Cu exchange equilibria between a-miargyrite, chalcostibite, pyrargyrite, and high-skinnerite: constraints on Ag-Cu in a-miargyrite and chalcostibite. Mineralogical Magazine, 63, 399-411.

  • Harlov, D. E. (1999): Thermochemistry of Ag-Cu exchange between proustite, sinnerite, and pearceite: constraints on Ag-Cu and As-Sb mixing in pyrargyrite-proustite. European Journal of Mineralogy, 11, 709-719.


  • Franz, L.; Harlov, D. E. (1998): High grade K-feldspar veining in granulites from the Ivrea-Verbano zone, Northern Italy: fluid flow in the lower crust and implications for granulite facies genesis. Journal of Geology, 106, 455-472.








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