Wordmark GFZ Potsdam

Publications

 
(Co) Author: Harlov, D. E.
  Paper (ISI journals)  
2012




2011


  • 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.
    | EDOC: 17905 | 10.1007/s00710-011-0166-6 | 







2010



  • 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.
    | EDOC: 16517 | 







2009

  • 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.
    | EDOC: 13187 | 10.1007/s00710-008-0033-2 | 


2008







2007



  • 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.
    | EDOC: 10126 | 





2006






2005






2004





2003

  • 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.
    | EDOC: 4061 | Abstract | 

  • 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.
    | EDOC: 3484 | Abstract | 


2002



  • 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.
    | EDOC: 2769 | 

  • 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.
    | EDOC: 2768 | 


  • 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.
    | EDOC: 3296 | 

  • 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.
    | EDOC: 2760 | 



2001





2000


  • 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.
    | EDOC: 345 | 

  • 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.
    | EDOC: 2175 | 

  • 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.
    | EDOC: 344 | 

  • 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.
    | EDOC: 343 | 


1999

  • 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.
    | EDOC: 1664 | 

  • 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.
    | EDOC: 347 | 

  • 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.
    | EDOC: 346 | 

1998

  • 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.
    | EDOC: 901 | 


1997


 TOP
  Paper (further journals)  
2002

  • Harlov, D. E. (2002): Review of petrographic and mineralogical evidence for fluid induced dehydration of amphibolite facies to granulite facies rocks. Zeitschrift für Geologische Wissenschaften, 30, 13-36.
    | EDOC: 3298 | 

 TOP
  Book  
2008

  • Harlov, D. E.; Broska, I. (Ed.) (2008): Mineral Equilibria, Metasomatism, and Mass Transport: Evolution and Stabilization of Rock on a Fluid-Rich World / (Ed.), Geological Institute, Slovak Academy of Sciences, 128.
    | EDOC: 12528 | 

 TOP
  Conference Paper  
2011

  • Harlov, D. E. (2011): Fluid-aided mineral breakdown, genesis, and re-equilibration during granulite-facies metamorphism: Natural and experimental evidence. AGU 2011 Fall Meeting (San Francisco, USA 2011).
    | EDOC: 18004 | 

  • Harlov, D. E. (2011): Fluids and charnockite formation during high-grade granulite-facies metamorphism in southern India. Joint Meeting DGK, DMG, ÖMG 'Crystals, Minerals and Materials' (Salzburg, Austria 2011), 11.
    | EDOC: 17435 | 

  • Harlov, D. E.; Thomas, J. B. (2011): The Role of Fluids, Melts, and Solid-State Diffusion During P-T-X Reequilibration Between Minerals in Metamorphic and Igneous Rocks Posters. AGU 2011 Fall Meeting (San Francisco, USA 2011).
    | EDOC: 18003 | 

  • Tropper, P.; Manning, C.; Harlov, D. E. (2011): Solubility measurements of CePO4 and YPO4 in H2O-NaF at 800°C and 1 GPa: implications for extremely high REE transport during granulite-facies metamorphism. Joint Meeting DGK, DMG, ÖMG 'Crystals, Minerals and Materials' (Salzburg, Austria 2011), 26.
    | EDOC: 17436 | 

2010





  • Norberg, N.; Neusser, G.; Harlov, D. E.; Abart, R. (2010): Reaction kinetics and alkali diffusion during replacement of K-rich alkali feldspars in (Na, K)Cl solutions. IMA 2010 - 20th General Meeting of the International Mineralogical Association (Budapest, Hungary 2010), 801.
    | EDOC: 15458 | 

2009

  • Harlov, D. E. (2009): Metasomatic alteration of monazite and xenotime in fluids: the role of coupled dissolution-reprecipitation vs. volume diffusion. MAPT: MicroAnalysis Processes Time - Annual Meeting of the Mineralogical Society of Great Britain and Ireland (Edinburgh, UK 2009), 91-92.
    | EDOC: 13638 | 

  • Harlov, D. E.; Hetherington, C. J. (2009): Metasomatic alteration of monazite: constraints on fluid chemistry and the dating of mass transport. General Assembly European Geosciences Union (Vienna, Austria 2009).
    | EDOC: 13181 | 


  • Norberg, N.; Neusser, G.; Rhede, D.; Harlov, D. E.; Abart, R. (2009): Microstructure evolution during hydrothermal replacement of potassium-rich alkali feldspars by high albite/high sanidine in aqueous NaCl/KCl solutions. 87. Jahrestagung der Deutschen Mineralogischen Gesellschaft (Halle/Saale 2009), 173.
    | EDOC: 13743 | 

  • Tropper, P.; Manning, C. E.; Harlov, D. E. (2009): Preliminary solubility measurements of CePO4 and YPO4 in H2O, H2O-NaCl, H2O-NaF, and H2O-Albite at 800°C and 1 GPa: Implications for the transport of REE during high-grade metamorphism. General Assembly European Geosciences Union (Vienna, Austria 2009).
    | EDOC: 13182 | 


2008

  • Budzyn, B.; Harlov, D. E. (2008): Formation of epidote-allanite solid solution and fluorapatite during experimental metasomatism of monazite under lower amphibolite-facies conditions. 12th International Conference on Experimental Mineralogy, Petrology and Geochemistry - EMPG XII - (Innsbruck, Austria 2008), 16.
    | EDOC: 11871 | 

  • Harlov, D. E. (2008): Metasomatic alteration of zircon in high pH fluids under high-grade conditions. General Assembly European Geosciences Union (Vienna, Austria 2008).
    | EDOC: 11244 | 

  • Harlov, D. E.; Budzyn, B. (2008): The stability of Cl-CO3-scapolite relative to plagioclase + CaCO3+CaSO4 in the presence of NaCl brines as a function of P-T-XNaCl. AGU 2008 Fall Meeting (San Francisco 2008).
    | EDOC: 12526 | 

  • Harlov, D. E.; Budzyn, B. (2008): The stability of CO3-scapolite (mizzonite) relative to plagioclase + CaCO3 + CaSO4 in the presence of a concentrated NaCl brine from 600-900°C and 500-1500 MPa. 12th International Conference on Experimental Mineralogy, Petrology and Geochemistry - EMPG XII - (Innsbruck, Austria 2008), 34.
    | EDOC: 11874 | 

  • Harlov, D. E.; Hetherington, C. (2008): Partial replacement of homogeneous monazite by monazite enriched in ThSiO4-CaTh(PO4)2 component: Nature and experiment. Mineral Equilibria, Metasomatism, and Mass Transport: Evolution and Stabilization of Rock on a Fluid-Rich World, MIMET 2008 Workshop (Smolenice, Slovak Republic 2008), 43-45.
    | EDOC: 12530 | 

  • Harlov, D. E.; Van den Kerkhof, A.; Johansson, L. (2008): Localised fluid-induced, solid state dehydration of amphibolite-facies to granulite-facies rock: the role of CO2-rich vs. concentrated NaCl/KCl brines. Mineral Equilibria, Metasomatism, and Mass Transport: Evolution and Stabilization of Rock on a Fluid-Rich World, MIMET 2008 Workshop (Smolenice, Slovak Republic 2008), 46-48.
    | EDOC: 12534 | 


  • Tropper, P.; Manning, C. E.; Harlov, D. E. (2008): Solubility of CePO4 and YPO4 in H2O, H2O-NaCl, H2O-NaF and H2O-Albite Fluids at 800°C and 1 GPa: Implications for REE transport during subduction-zone metasomatism. AGU 2008 Fall Meeting (San Francisco, USA 2008).
    | EDOC: 12527 | 

2007

  • Harlov, D. E. (2007): K-feldspar micro-veining in high-grade metamorphic rocks: fluids, melts, material transport, and mineral re-equilibration. Frontiers in Mineral Sciences 2007 (Cambridge, UK 2007), 218-219.
    | EDOC: 9892 | 

  • Harlov, D. E.; Hansen, E. C. (2007): Trends in phosphate and silicate mineral chemistry across a section of Archean crust, Tamil Nadu, south India: The role of fluids in regional granulite-facies metamorphism. General Assembly European Geoscience Union (EGU) (Vienna, Austria 2007).
    | EDOC: 9921 | 

  • Harlov, D. E.; Hetherington, C. (2007): Partial replacement of homogeneous monazite by monazite enriched in the ThSiO4-CaTh(PO4)2 component: nature and experiment. Frontiers in Mineral Sciences 2007 (Cambridge, UK 2007), 248-249.
    | EDOC: 9893 | 


  • Nijland, T. G.; Harlov, D. E. (2007): Selective joint-controlled oxide leaching in greenschist facies phyllites, Ottré, Ardennes, Belgium. General Assembly European Geoscience Union (EGU) (Vienna, Austria 2007).
    | EDOC: 9922 | 

2006

  • Hansen, E.; Harlov, D. E.; Thomason, C. (2006): Fluorapatite and biotite chemistry in orthopyroxene-bearing migmatites: Examples from California and southern India. 2006 Geological Society of America Annual Meeting (Philadelphia, USA 2006), 561.
    | EDOC: 9523 | 

  • Harlov, D. E. (2006): Fluid-rock interaction: mineral stability, mineral equilibria, and the propagation of metastable phases. AGU 2006 Fall Meeting (San Francisco, USA 2006).
    | EDOC: 9519 | 

  • Harlov, D. E. (2006): The role of apatite as a potential reservoir for the storage of Cl and F in the lower crust and upper mantle. 3rd General Assembly European Geosciences Union (Vienna, Austria 2006).
    | EDOC: 8655 | 

  • Harlov, D. E. (2006): The role of dissolution-reprecipitation in mineral equilibria during high-grade metamorphism. 2006 Geological Society of America Annual Meeting (Philadelphia, USA 2006), 112.
    | EDOC: 9520 | 

  • Harlov, D. E.; Hansen, E. C. (2006): Sulphide and oxide isograds along a late Archean, deep-crustal profile, Tamil Nadu, South India. 16th Annual VM Goldschmidt Conference (Melbourne, Australia 2006), A232.
    | EDOC: 9534 | 

  • Harlov, D. E.; Milke, R.; Gottschalk, M. (2006): Metastable reversal of sillimanite-corundum-quartz in the kyanite stability field: Competition between stable and metastable reactions. 2006 Geological Society of America Annual Meeting (Philadelphia, USA 2006), 169.
    | EDOC: 9522 | 


  • Tropper, P.; Harlov, D. E.; Krenn, E.; Finger, F.; Rhede, D.; Bernhard, F. (2006): Baddeleyite + W-bearing zirconolite + zircon-bearing veins as indicators for the polymetamorphic evolution of the eastern, lower Austroalpine nappes (Stubenberg Granite contact aureole, Styria, Eastern Alps, Austria). 3rd General Assembly European Geosciences Union (Vienna, Austria 2006).
    | EDOC: 8654 | 

2005



2004

  • Abart, R.; Harlov, D. E.; Podladchikov, Y. (2004): Clinopyroxene-scapolite symplectites at garnet-calcite interfaces: controls on pattern formation. 1st General Assembly European Geosciences Union (Nice, France 2004), EGU04-A-04803.
    | EDOC: 6408 | 

  • Hansen, E. C.; Harlov, D. E. (2004): Chemical and mineralogical patterns along a late-Archean crustal profile in southern India: signatures of a high temperature brine?. AGU 2004 Fall Meeting (San Francisco 2004), V31A-1408.
    | EDOC: 6091 | 

  • Harlov, D. E. (2004): Fluid induced dehydration of the mafic lower crust from amphibolite to granulite facies: nature and experiment. AGU 2004 Fall Meeting (San Francisco 2004), V31A-1409.
    | EDOC: 6089 | 

  • Harlov, D. E.; Abart, R. (2004): Experimental synthesis of simple symplectites in quartzo-feldspathic rocks: The role of fluids and melts. 1st General Assembly European Geosciences Union (Nice, France 2004), EGU04-A-05939.
    | EDOC: 6407 | 


  • Harlov, D. E.; Milke, R. (2004): Reversal of Sillimanite-Corundum-Quartz: Competition Between Stable and Metastable Reactions. 10th International Symposium on Experimental Mineralogy, Petrology and Geochemistry (Frankfurt/Main 2004), S48.
    | EDOC: 5181 | 

  • 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.
    | EDOC: 5521 | 

  • Montanini, A.; Harlov, D. E. (2004): Evidence for KCl metasomatism in mafic xenoliths from the lower crust. AGU 2004 Fall Meeting (San Francisco 2004), V31A-1410.
    | EDOC: 6090 | 

2003

  • 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.
    | EDOC: 3498 | 


  • 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).
    | EDOC: 4277 | 


2002

  • Harlov, D. E. (2002): Fluid induced dehydration of the mafic lower crust from amphibolite to granulite facies: nature and experiment. 9th International Symposium on Experimental Mineralogy, Petrology and Geochemistry (Zürich 2002), 43-44.
    | EDOC: 3301 | 

  • 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.
    | EDOC: 3302 | 

  • 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.
    | EDOC: 3299 | 

  • Harlov, D. E.; Milke, R. (2002): Reversal of sillimanite-corundum-quartz in the kyanite stability field: competition between stable and metastable reactions. 18th General Meeting of the International Mineralogical Association (Edinburgh 2002), 242.
    | EDOC: 3300 | 

  • Milke, R.; Harlov, D. E. (2002): Corundum + quartz = sillimanite and corundum + quartz = kyanite: Equilibria and competition between parallel reactions. 80. Jahrestagung der Deutschen Mineralogischen Gesellschaft (Hamburg 2002), 110.
    | EDOC: 7511 | 

2001

  • Andersson, U. B.; Harlov, D. E. (2001): Charnockite patches in a granite from central southern Sweden: a case of prograde charnockitization followed by rehydration to granite. European Union of Geosciences - EUG XI Meeting (Strasbourg 2001).
    | EDOC: 2706 | 

  • Harlov, D. E. (2001): Fluid induced dehydration of the mafic lower crust from amphibolite to granulite facies: nature and experiment. 79. Jahrestagung der Deutschen Mineralogischen Gesellschaft (Potsdam 2001), 73.
    | EDOC: 2771 | 


  • 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.
    | EDOC: 2773 | 

  • 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.
    | EDOC: 2772 | 

2000


  • 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.
    | EDOC: 1669 | 

  • 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.
    | EDOC: 1671 | 

  • Harlov, D. E.; Melzer, S. (2000): Rb-K Exchange between phlogopite and low H2O activity (K,Rb)Cl brines at high pressure and temperature: implications for the role of supercritical KCl brines in the depletion of Rb during charnockite genesis. 8th International Symposium on Experimental Mineralogy, Petrology and Geochemistry (Bergamo 2000), 46.
    | EDOC: 2117 | 

  • Harlov, D. E.; Melzer, S.; Hansen, E. C. (2000): Rb-K exchange between phlogopite and low H2O activity (K,Rb)Cl brines at high pressures and temperature: implications for the role of supercritical KCl brines in the depletion of Rb during charnockite genesis. Annual Meeting Geological Society of America (Reno 2000), A152.
    | EDOC: 2118 | 



1999


  • 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).
    | EDOC: 1675 | 

  • 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.
    | EDOC: 1672 | 

  • Harlov, D. E.; Gottschalk, M.; Heinrich, W. (1999): Stability of NH4-silicate minerals at high temperatures and pressures buffered to Ni-NiO oxygen fugacity. 77. Jahrestagung der Deutschen Mineralogischen Gesellschaft (Wien 1999), 97.
    | EDOC: 2258 | 

1998

  • Andrut, M.; Gottschalk, M.; Harlov, D. E. (1998): NH4+ fundamentals, overtones and combination modes in buddingtonite. 7th International Symposium on Experimental Mineralogy, Petrology and Geochemistry (Orléans 1998).
    | EDOC: 2735 | 

  • 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).
    | EDOC: 1677 | 

  • Harlov, D. E.; Gottschalk, M.; Heinrich, W. (1998): Stability of NH4-silicate minerals at high temperatures, pressures and oxygen fugacities. 7th International Symposium on Experimental Mineralogy, Petrology and Geochemistry (Orléans 1998), 24.
    | EDOC: 2431 | 

1997

  • Franz, L.; Harlov, D. E. (1997): Indikationen für kaliumreiches Fluid während der Genese der Granulite in der Ivrea-Verbano Zone (Norditalien). 75. Jahrestagung der Deutschen Mineralogischen Gesellschaft (Köln 1997), 107.
    | EDOC: 7442 | 

  • Hansen, E. C.; Harlov, D. E.; Bigler, C. (1997): Non-silicate mineralogy and mineral chemistry along a late Archean deep-crustal profile in South India. Annual Meeting Geological Society of America (Salt Lake City 1997), 398.
    | EDOC: 7443 | 

  • Harlov, D. E.; Franz, L. (1997): Evidence for K-rich fluids during the genesis of granulites from the Ivrea-Verbano zone, northern Italy. 7th Annual Goldschmidt Conference (Houston, USA 1997), 87-88.
    | EDOC: 7444 | 

  • Harlov, D. E.; Franz, L. (1997): Role of fluids in the genesis of granulites from the Ivrea-Verbano zone, northern Italy: comparisons with Precambrian granulites. European Union of Geosciences (EUG-9) (Strasbourg 1997), 364.
    | EDOC: 7445 | 

  • Harlov, D. E.; Heinrich, W.; Gottschalk, M. (1997): Experimental calibration of the equilibrium: 6 buddingtonite + 3 O2 -><- 2 tobelite + 12 Quartz + 2 N2 + 6 H2O at 2 and 4 kilobars buffered to Mt-Hm fO2. Meeting 'Mineral equilibria and databases' (Espoo, Finnland 1997), 37-38.
    | EDOC: 2746 | 

  • Harlov, D. E.; Heinrich, W.; Gottschalk, M. (1997): Experimental calibration of the equilibrium: 6 buddingtonite + 3 O2 = 2 tobelite + 12 quartz + 2 N2 + 6 H2O at 2 and 4 kbars buffered to Mt-Hm fO2. 75. Jahrestagung der Deutschen Mineralogischen Gesellschaft (Köln 1997), 144.
    | EDOC: 2429 | 

  • Harlov, D. E.; Heinrich, W.; Gottschalk, M. (1997): Experimental calibration of the equilibrium: 6 buddingtonite + 3 O2 = 2 tobelite + 12 quartz + 2 N2 + 6 H2O at 2 kilobars. 7th Annual Goldschmidt Conference (Houston, USA 1997), 88.
    | EDOC: 2420 | 

  • Harlov, D. E.; Heinrich, W.; Gottschalk, M. (1997): Experimental calibration of the equilibrium: 6 buddingtonite + 3O2 -><- 2 tobelite + 12 Quartz + 2N2 + 6H2O at 2 and 4 kilobars buffered to Mt-Hm fO2. 75. Jahrestagung der Deutschen Mineralogischen Gesellschaft (Köln 1997), 144.
    | EDOC: 2747 | 

1996



 TOP




  to top