Jiu-shuai Deng, Shu-ming Wen, Dan-dan Wu, Jian Liu, Xiao-lin Zhang, and Hai-ying Shen, Existence and release of fluid inclusions in bornite and its associated quartz and calcite, Int. J. Miner. Metall. Mater., 20(2013), No. 9, pp. 815-822. https://doi.org/10.1007/s12613-013-0801-9
Cite this article as:
Jiu-shuai Deng, Shu-ming Wen, Dan-dan Wu, Jian Liu, Xiao-lin Zhang, and Hai-ying Shen, Existence and release of fluid inclusions in bornite and its associated quartz and calcite, Int. J. Miner. Metall. Mater., 20(2013), No. 9, pp. 815-822. https://doi.org/10.1007/s12613-013-0801-9
Jiu-shuai Deng, Shu-ming Wen, Dan-dan Wu, Jian Liu, Xiao-lin Zhang, and Hai-ying Shen, Existence and release of fluid inclusions in bornite and its associated quartz and calcite, Int. J. Miner. Metall. Mater., 20(2013), No. 9, pp. 815-822. https://doi.org/10.1007/s12613-013-0801-9
Citation:
Jiu-shuai Deng, Shu-ming Wen, Dan-dan Wu, Jian Liu, Xiao-lin Zhang, and Hai-ying Shen, Existence and release of fluid inclusions in bornite and its associated quartz and calcite, Int. J. Miner. Metall. Mater., 20(2013), No. 9, pp. 815-822. https://doi.org/10.1007/s12613-013-0801-9
The existence and release of fluid inclusions in bornite and its associated minerals, namely, quartz and calcite were investigated and confirmed. The structures, forms, and phases of these large quantities of fluid inclusions were also studied. A mass of fluid inclusions with various sizes, distributions, shapes, and phases exist in bornite and its associated minerals. Their sizes vary from a few micrometers to tens of micrometers, and the forms appear as negative crystals, or elongated, elliptical, and irregular. At room temperature, fluid inclusions were mainly characterized as gas-liquid twophase. However, small amounts of fluid inclusions with pure gas phase and pure liquid single-phase were also observed in quartz and calcite. These fluid inclusions initially broke during the ore crushing and grinding process and then released into the flotation pulp in the flotation process. The quantitative analysis of fluid inclusions in the solution and the comparisons of mineral dissolution show that the amount of copper and iron released by fluid inclusions in the bornite sample is higher than the amount dissolved by the mineral; fluid inclusions in the associated gangue minerals, quartz, and calcite also make contribution.
The existence and release of fluid inclusions in bornite and its associated minerals, namely, quartz and calcite were investigated and confirmed. The structures, forms, and phases of these large quantities of fluid inclusions were also studied. A mass of fluid inclusions with various sizes, distributions, shapes, and phases exist in bornite and its associated minerals. Their sizes vary from a few micrometers to tens of micrometers, and the forms appear as negative crystals, or elongated, elliptical, and irregular. At room temperature, fluid inclusions were mainly characterized as gas-liquid twophase. However, small amounts of fluid inclusions with pure gas phase and pure liquid single-phase were also observed in quartz and calcite. These fluid inclusions initially broke during the ore crushing and grinding process and then released into the flotation pulp in the flotation process. The quantitative analysis of fluid inclusions in the solution and the comparisons of mineral dissolution show that the amount of copper and iron released by fluid inclusions in the bornite sample is higher than the amount dissolved by the mineral; fluid inclusions in the associated gangue minerals, quartz, and calcite also make contribution.
下载: