• A MODEL FOR THE STRUCTURE OF THE HYDRATED ALUMINUM PHOSPHATE, KINGITE DETERMINED BY AB INITIO POWDER DIFFRACTION METHODS 

  Wallwork K.S.; Pring A.; Taylor M.R.; Hunter B.A. (2003)

  The crystal structure of kingite, Al3(PO4)2(F,OH)2·8(H2O,OH), a secondary mineral from a Cambrian-Precambrian phosphate deposit at Tom’s Quarry, near Kapunda, South Australia, has been determined from a powder sample using ...
• CALIBRATION OF METHANE ANALYSIS BY RAMAN SPECTROSCOPY IN H2O-NACL-CH4 FLUID INCLUSIONS 

  Guillaume D.; Teinturier S.; Dubessy J.; Pironon J. (2003)

  Calibration of the determination of CH4/H2O ratio using Raman spectroscopy is carried out using synthetic fluid inclusions at different NaCl concentration (0, 0.05, 0.66, 0.98, 1.00, 1.60, 2.25 and 3.5 m NaCl). Spectra of ...
• A REFINED SOLUTION TO THE FIRST TERRESTRIAL PB-ISOTOPE PARADOX 

  Murphy D.T.; Kamber B.S.; Collerson K.D. (2003)

  The first terrestrial Pb-isotope paradox refers to the fact that on average, rocks from the Earth's surface (i.e. the accessible Earth) plot significantly to the right of the meteorite isochron in a common Pb-isotope ...
• PERTSEVITE, A NEW SILICATIAN MAGNESIOBORATE MINERAL WITH AN END-MEMBER COMPOSITION MG2BO3F, IN KOTOITE MARBLE FROM EAST OF VERKHOYANSK, SAKHA-YAKUTIA, RUSSIA 

  Schreyer W.; Bernhardt H.; Medenbach O.; Armbruster T. (2003)

  Pertsevite is a new Mg borate from a contact-metasomatic kotoite marble from the region east of Verkhoyansk, Sakha-Yakutia, northeastern Siberia. The end member is defined as Mg2BO3F, which is the composition of a synthetic ...
• SPECTROSCOPIC 2D-TOMOGRAPHY: RESIDUAL PRESSURE AND STRAIN AROUND MINERAL INCLUSIONS IN DIAMONDS 

  Nasdala L.; Hofmeister W.; Brenker F.E.; Glinnemann J.; Gasparik T.; Harris J.W.; Stachel T.; Reese I. (2003)

  We have studied high-pressure inclusions (Ca-silicates, coesite, graphite) in three large diamonds, one from the Kankan district, Guinea, and the other two from the Panda kimberlite, Ekati diamond mines, Canada. Using the ...

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