The metal-rich portions of the phase system Cu-Fe-Pd-S at 1000 degrees C, 900 degrees C, and 725 degrees C: implications for mineralization in the Skaergaard intrusion

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Standard

The metal-rich portions of the phase system Cu-Fe-Pd-S at 1000 degrees C, 900 degrees C, and 725 degrees C : implications for mineralization in the Skaergaard intrusion. / Karup-Møller, Sven; Makovicky, Emil; Barnes, Sarah Jane.

I: Mineralogical Magazine, Bind 72, 2008, s. 941-951.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Karup-Møller, S, Makovicky, E & Barnes, SJ 2008, 'The metal-rich portions of the phase system Cu-Fe-Pd-S at 1000 degrees C, 900 degrees C, and 725 degrees C: implications for mineralization in the Skaergaard intrusion', Mineralogical Magazine, bind 72, s. 941-951. https://doi.org/10.1180/minmag.2008.072.4.941

APA

Karup-Møller, S., Makovicky, E., & Barnes, S. J. (2008). The metal-rich portions of the phase system Cu-Fe-Pd-S at 1000 degrees C, 900 degrees C, and 725 degrees C: implications for mineralization in the Skaergaard intrusion. Mineralogical Magazine, 72, 941-951. https://doi.org/10.1180/minmag.2008.072.4.941

Vancouver

Karup-Møller S, Makovicky E, Barnes SJ. The metal-rich portions of the phase system Cu-Fe-Pd-S at 1000 degrees C, 900 degrees C, and 725 degrees C: implications for mineralization in the Skaergaard intrusion. Mineralogical Magazine. 2008;72:941-951. https://doi.org/10.1180/minmag.2008.072.4.941

Author

Karup-Møller, Sven ; Makovicky, Emil ; Barnes, Sarah Jane. / The metal-rich portions of the phase system Cu-Fe-Pd-S at 1000 degrees C, 900 degrees C, and 725 degrees C : implications for mineralization in the Skaergaard intrusion. I: Mineralogical Magazine. 2008 ; Bind 72. s. 941-951.

Bibtex

@article{bd4ba6c0d81811dea1f3000ea68e967b,
title = "The metal-rich portions of the phase system Cu-Fe-Pd-S at 1000 degrees C, 900 degrees C, and 725 degrees C: implications for mineralization in the Skaergaard intrusion",
abstract = "The sulphur-poor portions of the dry condensed Cu-Fe-Pd-S system were studied at 1000ºC, 900ºC and 725ºC by synthesis in evacuated silicate glass tubes, along with textural observations and electron microprobe analyses of equilibrated reaction products. Sulphide melt coexists with Cu-Fe-Pd alloys, bornite, Fe1-xS and iss (intermediate solid solution, Cabri, 1973) and Pd4S. Compositional data were obtained for the associations bornite-alloy-melt, pyrrhotite-alloy-melt and for immiscible Cu-rich sulphide melts. Partition coefficients for all three metals were derived for the association alloy-melt. Formation of the two new Cu-Pd alloy minerals, skaergaardite and nielsenite, is discussed in terms of the present findings",
keywords = "Faculty of Science, Cu-Pd-Fe-S phase system, nielsenite, skaergaardite, bornite, Cu-Pd-Fe alloy, sulphide melt",
author = "Sven Karup-M{\o}ller and Emil Makovicky and Barnes, {Sarah Jane}",
year = "2008",
doi = "10.1180/minmag.2008.072.4.941",
language = "English",
volume = "72",
pages = "941--951",
journal = "Mineralogical Magazine",
issn = "0026-461X",
publisher = "Mineralogical Society",

}

RIS

TY - JOUR

T1 - The metal-rich portions of the phase system Cu-Fe-Pd-S at 1000 degrees C, 900 degrees C, and 725 degrees C

T2 - implications for mineralization in the Skaergaard intrusion

AU - Karup-Møller, Sven

AU - Makovicky, Emil

AU - Barnes, Sarah Jane

PY - 2008

Y1 - 2008

N2 - The sulphur-poor portions of the dry condensed Cu-Fe-Pd-S system were studied at 1000ºC, 900ºC and 725ºC by synthesis in evacuated silicate glass tubes, along with textural observations and electron microprobe analyses of equilibrated reaction products. Sulphide melt coexists with Cu-Fe-Pd alloys, bornite, Fe1-xS and iss (intermediate solid solution, Cabri, 1973) and Pd4S. Compositional data were obtained for the associations bornite-alloy-melt, pyrrhotite-alloy-melt and for immiscible Cu-rich sulphide melts. Partition coefficients for all three metals were derived for the association alloy-melt. Formation of the two new Cu-Pd alloy minerals, skaergaardite and nielsenite, is discussed in terms of the present findings

AB - The sulphur-poor portions of the dry condensed Cu-Fe-Pd-S system were studied at 1000ºC, 900ºC and 725ºC by synthesis in evacuated silicate glass tubes, along with textural observations and electron microprobe analyses of equilibrated reaction products. Sulphide melt coexists with Cu-Fe-Pd alloys, bornite, Fe1-xS and iss (intermediate solid solution, Cabri, 1973) and Pd4S. Compositional data were obtained for the associations bornite-alloy-melt, pyrrhotite-alloy-melt and for immiscible Cu-rich sulphide melts. Partition coefficients for all three metals were derived for the association alloy-melt. Formation of the two new Cu-Pd alloy minerals, skaergaardite and nielsenite, is discussed in terms of the present findings

KW - Faculty of Science

KW - Cu-Pd-Fe-S phase system

KW - nielsenite

KW - skaergaardite

KW - bornite

KW - Cu-Pd-Fe alloy

KW - sulphide melt

U2 - 10.1180/minmag.2008.072.4.941

DO - 10.1180/minmag.2008.072.4.941

M3 - Journal article

VL - 72

SP - 941

EP - 951

JO - Mineralogical Magazine

JF - Mineralogical Magazine

SN - 0026-461X

ER -

ID: 15998225