Journal & Issues

Volume 54 (2023): Issue 1 (January 2023)

Volume 53 (2022): Issue 1 (January 2022)

Volume 52 (2021): Issue 1 (January 2021)

Volume 51 (2020): Issue 1 (January 2020)

Volume 50 (2019): Issue 1-4 (December 2019)

Volume 49 (2018): Issue 1-4 (December 2018)

Volume 48 (2017): Issue 1-4 (December 2017)

Volume 47 (2016): Issue 1-4 (December 2016)

Volume 46 (2015): Issue 1-2 (June 2015)

Volume 45 (2014): Issue 3-4 (December 2014)

Volume 45 (2015): Issue 1-2 (June 2015)

Volume 44 (2013): Issue 3-4 (July 2013)

Volume 44 (2013): Issue 1-2 (June 2013)

Volume 43 (2012): Issue 3-4 (December 2012)

Volume 43 (2012): Issue 1-2 (March 2012)

Volume 42 (2012): Issue 4 (October 2012)

Volume 42 (2011): Issue 2-3 (January 2011)

Volume 42 (2011): Issue 1 (January 2011)

Volume 41 (2010): Issue 3-4 (January 2010)

Volume 41 (2010): Issue 1-2 (January 2010)

Volume 40 (2009): Issue 1-4 (January 2009)

Volume 39 (2008): Issue 3-4 (January 2008)

Volume 39 (2008): Issue 1-2 (January 2008)

Volume 38 (2007): Issue 2 (January 2007)

Volume 38 (2007): Issue 1 (January 2007)

Volume 37 (2006): Issue 2 (January 2006)

Volume 37 (2006): Issue 1 (January 2006)

Journal Details
Format
Journal
eISSN
1899-8526
First Published
05 Feb 2007
Publication timeframe
1 time per year
Languages
English

Search

Volume 50 (2019): Issue 1-4 (December 2019)

Journal Details
Format
Journal
eISSN
1899-8526
First Published
05 Feb 2007
Publication timeframe
1 time per year
Languages
English

Search

0 Articles
Open Access

Synthesis and characterization of cadmium chlorapatite Cd5(PO4)3Cl

Published Online: 03 Apr 2020
Page range: 3 - 12

Abstract

Abstract

One of the most effective methods for the immobilization of toxic metals involves the use of minerals from the apatite supergroup. The formation of cadmium chlorapatite may lead to successful entrapping of cadmium; thus, it is important to examine the solubility constant to determine the stability of cadmium in the the apatite structure. Cadmium chlorapatite was synthetized and characterized by X-ray diffraction, infrared spectroscopy, Raman spectroscopy, and scanning electron microscopy. The solubility constant (log) Ksp of cadmium chlorapatite was -65.58. The Gibbs free energy of formation of cadmium chlorapatite reached -3950.48 kJ mol−1. The solubility constant turned out to be low but was enough for cadmium chlorapatiteto be considered a very stable compound..

Keywords

  • Apatite
  • Cadmium
  • Cadmium chloroapatite
  • Dissolution
  • Solubility constant
Open Access

Lamprophyric rock locations in Greece

Published Online: 03 Apr 2020
Page range: 13 - 33

Abstract

Abstract

Twenty-four areas with lamprophyric formations have been located through a bibliographic search in Macedonia, Thrace, the islands and Attica. Most lamprophyre types have been identified including rare “alkali minette”. In most localities the dikes/sills appear to be late mantle products associated with deep faulting following extensional activity in granitoids.

Keywords

  • lamprophyric rocks
  • distribution
  • Greece
  • bibliography
Open Access

Geochemistry, mineral chemistry and P-T evaluation of metasediments of Bahram-Gur complex, ES Sanandaj-Sirjan zone, Iran

Published Online: 03 Apr 2020
Page range: 34 - 68

Abstract

Abstract

The Bahram-Gur area in the southeastern part of the Sanandaj – Sirjan metamorphic zone, contains metabasites and metasediments. The metasedimentary rocks are mainly garnet schists and garnet-staurolite schists that were metamorphosed under amphibolite facies conditions. The rocks consist of garnet ± staurolite, biotite, muscovite, chlorite and quartz. The geochemistry of the Bahram-Gur metasediments classifies them as quartziferous sedimentary rocks. The protoliths of the metasedimentary rocks were close to greywackes from an ensialic arc basin depositional setting, with a source comprising mostly mixture of acid and intermediate magmatic rocks in the upper continental crust. The metamorphic conditions of formation of the Bahram-Gur metasedimentary are investigated by geothermobarometric methods. The results show that the metasedimentary rocks formed at temperatures of 600-750°C and pressures of 5-7.5 kbar.

Keywords

  • Bahram-Gur area
  • Sanandaj-Sirjan Zone
  • metamorphic conditions
  • metasediments
  • geothermobarometry
0 Articles
Open Access

Synthesis and characterization of cadmium chlorapatite Cd5(PO4)3Cl

Published Online: 03 Apr 2020
Page range: 3 - 12

Abstract

Abstract

One of the most effective methods for the immobilization of toxic metals involves the use of minerals from the apatite supergroup. The formation of cadmium chlorapatite may lead to successful entrapping of cadmium; thus, it is important to examine the solubility constant to determine the stability of cadmium in the the apatite structure. Cadmium chlorapatite was synthetized and characterized by X-ray diffraction, infrared spectroscopy, Raman spectroscopy, and scanning electron microscopy. The solubility constant (log) Ksp of cadmium chlorapatite was -65.58. The Gibbs free energy of formation of cadmium chlorapatite reached -3950.48 kJ mol−1. The solubility constant turned out to be low but was enough for cadmium chlorapatiteto be considered a very stable compound..

Keywords

  • Apatite
  • Cadmium
  • Cadmium chloroapatite
  • Dissolution
  • Solubility constant
Open Access

Lamprophyric rock locations in Greece

Published Online: 03 Apr 2020
Page range: 13 - 33

Abstract

Abstract

Twenty-four areas with lamprophyric formations have been located through a bibliographic search in Macedonia, Thrace, the islands and Attica. Most lamprophyre types have been identified including rare “alkali minette”. In most localities the dikes/sills appear to be late mantle products associated with deep faulting following extensional activity in granitoids.

Keywords

  • lamprophyric rocks
  • distribution
  • Greece
  • bibliography
Open Access

Geochemistry, mineral chemistry and P-T evaluation of metasediments of Bahram-Gur complex, ES Sanandaj-Sirjan zone, Iran

Published Online: 03 Apr 2020
Page range: 34 - 68

Abstract

Abstract

The Bahram-Gur area in the southeastern part of the Sanandaj – Sirjan metamorphic zone, contains metabasites and metasediments. The metasedimentary rocks are mainly garnet schists and garnet-staurolite schists that were metamorphosed under amphibolite facies conditions. The rocks consist of garnet ± staurolite, biotite, muscovite, chlorite and quartz. The geochemistry of the Bahram-Gur metasediments classifies them as quartziferous sedimentary rocks. The protoliths of the metasedimentary rocks were close to greywackes from an ensialic arc basin depositional setting, with a source comprising mostly mixture of acid and intermediate magmatic rocks in the upper continental crust. The metamorphic conditions of formation of the Bahram-Gur metasedimentary are investigated by geothermobarometric methods. The results show that the metasedimentary rocks formed at temperatures of 600-750°C and pressures of 5-7.5 kbar.

Keywords

  • Bahram-Gur area
  • Sanandaj-Sirjan Zone
  • metamorphic conditions
  • metasediments
  • geothermobarometry