Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Stamatis Flemetakis"'
Publikováno v:
Contributions to Mineralogy and Petrology. 177
We present new experimental data on the effect of F on the stability of antigorite and its breakdown products at high pressures (2–6 GPa) and high temperatures (570–850 °C). The experiments show that F does not affect the stability of antigorite
Autor:
R. van Mulligen, W. van Westrenen, Stamatis Flemetakis, F. van Haaster, Stephan Klemme, Edgar S. Steenstra, Jasper Berndt
Publikováno v:
Steenstra, E S, van Haaster, F, van Mulligen, R, Flemetakis, S, Berndt, J, Klemme, S & van Westrenen, W 2020, ' An experimental assessment of the chalcophile behavior of F, Cl, Br and I : Implications for the fate of halogens during planetary accretion and the formation of magmatic ore deposits ', Geochimica et Cosmochimica Acta, vol. 273, pp. 275-290 . https://doi.org/10.1016/j.gca.2020.01.006
Geochimica et Cosmochimica Acta, 273, 275-290. Elsevier Limited
Geochimica et Cosmochimica Acta, 273, 275-290. Elsevier Limited
The elemental and isotopic abundances of halogens (F, Cl, Br, I) are used to constrain planetary volatile loss and volatile delivery processes, but their behavior during magmatic differentiation in general, and sulfide liquid segregation in particula
Autor:
Stamatis Flemetakis, Stamatios Xydous, Stephan Klemme, Jasper Berndt, Constantinos Mavrogonatos, Ioannis Baziotis, Paul D. Asimow
Publikováno v:
Geochimica et Cosmochimica Acta. 266:307-331
We investigate the potential to use concentrations and zoning patterns of phosphorus (P) in clinopyroxene as indicators of the rates of igneous and metasomatic processes, comparable to recent applications of P in olivine but applicable to more evolve
Autor:
Anita Cadoux, Stamatis Flemetakis, Felix S. Genske, Jasper Berndt, Arno Rohrbach, Stephan Klemme, Marion Louvel
Publikováno v:
Microscopy and microanalysis : the official journal of Microscopy Society of America, Microbeam Analysis Society, Microscopical Society of Canada. 26(5)
We present a new analytical method, which allows the simultaneous analysis of fluorine (F), chlorine (Cl), bromine (Br), and iodine (I) in geological samples. To account for interferences of Fe on the spectral lines of F, of Al on Br-lines, and of Ca
Autor:
Stephan Klemme, Stamatis Xydous, Ioannis Baziotis, Paul D. Asimow, Angeliki Papoutsa, Stamatis Flemetakis, Jasper Berndt, Constantinos Mavrogonatos
Phosphorus(P)-rich zones in olivine may reflect incorporation of P in excess of equilibrium partitioning during rapid growth (e.g. Milman-Barris et al. 2008). We investigated (by optical microscopy and electron microprobe) a composite mantle xenolith
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2273f6640a80a7f46f70a36a72200f80
https://doi.org/10.5194/egusphere-egu2020-7207
https://doi.org/10.5194/egusphere-egu2020-7207
Autor:
Stamatis Flemetakis, Arno Rohrbach, Felix S. Genske, Stephan Klemme, Andreas Stracke, Jasper Berndt
Publikováno v:
Lithos. :105859
We present experimentally determined partition coefficients (Dmin/melt) for F and Cl between pargasite (amphibole), phlogopite (mica), clinopyroxene and basanitic melts. All experiments were performed at 1.4 GPa and temperatures between 1015 °C and
Autor:
Stamatis Flemetakis, Felix S. Genske, Jasper Berndt, Anita Cadoux, Arno Rohrbach, Marion Louvel, Stephan Klemme
Publikováno v:
Microscopy and Microanalysis. 26:1076-1076
Autor:
Ioannis Baziotis, Panagiotis Voudouris, Jasper Berndt, Constantinos Mavrogonatos, Stephan Klemme, Stamatios Xydous, Stamatis Flemetakis
Publikováno v:
Minerals
Volume 8
Issue 11
Minerals, Vol 8, Iss 11, p 487 (2018)
Volume 8
Issue 11
Minerals, Vol 8, Iss 11, p 487 (2018)
The color of quartz and other minerals can be either caused by defects in the crystal structure or by finely dispersed inclusions of other minerals within the crystals. In order to investigate the mineral chemistry and genesis of the famous prase (gr