A High Temperature and High Pressure Experimental Study on Re-Bearing Capability of Sulfide

Yingying Liu; Zhilong Huang; Chengming Zhu

doi:10.1007/s12583-017-0739-3

Volume 28 Issue 1

Feb 2017

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Journal of Earth Science > 2017 > 28(1): 78-91.

Yingying Liu, Zhilong Huang, Chengming Zhu. A High Temperature and High Pressure Experimental Study on Re-Bearing Capability of Sulfide. Journal of Earth Science, 2017, 28(1): 78-91. doi: 10.1007/s12583-017-0739-3

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Yingying Liu, Zhilong Huang, Chengming Zhu. A High Temperature and High Pressure Experimental Study on Re-Bearing Capability of Sulfide. Journal of Earth Science, 2017, 28(1): 78-91. doi: 10.1007/s12583-017-0739-3

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A High Temperature and High Pressure Experimental Study on Re-Bearing Capability of Sulfide

doi: 10.1007/s12583-017-0739-3

1.
State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
2.
Key Laboratory for High Temperature & High Pressure Study of the Earthos Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China

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Author Bio:
Yingying Liu: http://orcid-org/0000-0003-2656-2514

Zhilong Huang: http://orcid-org/0000-0002-4062-5107
Corresponding author: Zhilong Huang, huangzhilong@vip.gyig.ac.cn
Received Date: 17 Sep 2015
Accepted Date: 02 Dec 2015
Publish Date: 01 Feb 2017

Abstract

Abstract

High temperature (1 270Ƀ1 550 ¦) and high pressure (1.0 GPa) experimental studies on Re-bearing capabilities of pyrite, galena and sphalerite from typical Pb-Zn ore deposits were performed on a six-anvil apparatus. We observed microstructures of the quenched sulfides using scanning electron microscope (SEM) and analyzed compositions of the run products using both energy disperse spectroscopy (EDS) and electron probe microanalyzer (EPMA). The results show that pyrite melt can dissolve much more metallic Re than galena and sphalerite melts, forming scattered acicular ReS₂ in the quenched matrix of pyrrhotite (Fe_1-xS). The quenched matrixes of Fe_1-xS, PbS and ZnS generally contain less than 1.0 wt.% of Re and their Re-bearing capabilities seem to range as Fe_1-xS > PbS > ZnS. However, Re partition coefficients between them are difficult to estimate, because Re distribution is inhomogeneous in the quenched sulfide matrixes.
- pyrite,
- galena,
- sphalerite,
- high P-T experiment,
- Re-bearing capability

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References(86)

References

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