REE mobility during hydrothermal ore-forming processes has been extensively investigated in recent years and the potential of REE to provide information about ore forming processes has commonly been recognized. The Do...REE mobility during hydrothermal ore-forming processes has been extensively investigated in recent years and the potential of REE to provide information about ore forming processes has commonly been recognized. The Dongping gold deposit, which is located in northwestern Hebei Province, China, occurring in the inner contact zone of the Shuiquangou syenite complex, is spatially, and probably genetically, related to the syenite. The deposit was formed under the moderate to high temperature (220℃ to 320℃), weakly acidic to weakly alkaline, rather high f O 2 (lgf O 2=-30 ～- 34) environment. The REE study of the host rocks, altered wall rocks, ores and gangue minerals from the deposit suggests that the REEs have been mobilized and differentiated during K-feldspathization and silicification. The extremely altered syenite enveloping auriferous quartz vein shows positive Ce anomaly and larger LREE/HREE ratio than that of the unaltered syenite. The REE concentrations and patterns of the ores are determined by the ore types and mineral assemblages. LREE/HREE ratios in the gangue quartz and hydrothermal K-feldspars are relatively low. The most significant observation is that the gangue quartz shows significant positive Eu anomaly, whereas the hydrothermal K-feldspars show less significant or no positive Eu anomaly at all relative to the primary feldspar in the unaltered syenite. It is evident that the REEs are mobile during K-feldspathization and silicification in the ore forming process. Weak to moderate K-feldspathization caused REE mobility without apparent differentiation with the exception of extreme K-feldspathization and silicification which resulted in significant depletion of HREE and Eu and relative enrichment of Ce. The REE, Y, U, Th and Au contents of the syenite decrease as the degrees of K-feldspathization and silicification of the rocks increase towards the auriferous quartz veins. As the ores were deposited under a rather oxidized environment, Ce 4+ predominated over Ce 3+. The precipitation of the form展开更多
The as-sintered sinter skin of WC-11Co-0.71Cr3C2-0.06RE cemented carbide with WC＋βmicrostructure was analyzed by scanning electron microscope, energy dispersive X-ray spectroscope and X-ray diffractometer. RE repres...The as-sintered sinter skin of WC-11Co-0.71Cr3C2-0.06RE cemented carbide with WC＋βmicrostructure was analyzed by scanning electron microscope, energy dispersive X-ray spectroscope and X-ray diffractometer. RE represents La-, Ce-, Pr- and Nd-containing mischmetal, andβis cobalt-based binder phase. It was discovered that La, Ce, Pr and Nd migrated directionally from the alloy to the sinter skin to combine with the impurity elements S and O from the sintering atmosphere during the sintering process. As a result, main dispersed phase RE2S3 and minor RE2O2S were formed in situ on the sinter skin. The mechanisms for the stimulation of the migration activity and the directional migration of RE atoms were discussed in terms of the thermodynamics stability of Cr3C2, solubility characteristic of Cr in Co and the polarization or ionization of RE atoms.展开更多
文摘REE mobility during hydrothermal ore-forming processes has been extensively investigated in recent years and the potential of REE to provide information about ore forming processes has commonly been recognized. The Dongping gold deposit, which is located in northwestern Hebei Province, China, occurring in the inner contact zone of the Shuiquangou syenite complex, is spatially, and probably genetically, related to the syenite. The deposit was formed under the moderate to high temperature (220℃ to 320℃), weakly acidic to weakly alkaline, rather high f O 2 (lgf O 2=-30 ～- 34) environment. The REE study of the host rocks, altered wall rocks, ores and gangue minerals from the deposit suggests that the REEs have been mobilized and differentiated during K-feldspathization and silicification. The extremely altered syenite enveloping auriferous quartz vein shows positive Ce anomaly and larger LREE/HREE ratio than that of the unaltered syenite. The REE concentrations and patterns of the ores are determined by the ore types and mineral assemblages. LREE/HREE ratios in the gangue quartz and hydrothermal K-feldspars are relatively low. The most significant observation is that the gangue quartz shows significant positive Eu anomaly, whereas the hydrothermal K-feldspars show less significant or no positive Eu anomaly at all relative to the primary feldspar in the unaltered syenite. It is evident that the REEs are mobile during K-feldspathization and silicification in the ore forming process. Weak to moderate K-feldspathization caused REE mobility without apparent differentiation with the exception of extreme K-feldspathization and silicification which resulted in significant depletion of HREE and Eu and relative enrichment of Ce. The REE, Y, U, Th and Au contents of the syenite decrease as the degrees of K-feldspathization and silicification of the rocks increase towards the auriferous quartz veins. As the ores were deposited under a rather oxidized environment, Ce 4+ predominated over Ce 3+. The precipitation of the form
基金Project(51074189)supported by the National Natural Science Foundation of ChinaProject(2012ZX04003–021)supported by the National Science&Technology Special Foundation of ChinaProject(Y2012–010)supported by the Nonferrous Metals Research Foundation from Hunan Nonferrous Metals Holding Group Co.,Ltd.–CSU,China
文摘The as-sintered sinter skin of WC-11Co-0.71Cr3C2-0.06RE cemented carbide with WC＋βmicrostructure was analyzed by scanning electron microscope, energy dispersive X-ray spectroscope and X-ray diffractometer. RE represents La-, Ce-, Pr- and Nd-containing mischmetal, andβis cobalt-based binder phase. It was discovered that La, Ce, Pr and Nd migrated directionally from the alloy to the sinter skin to combine with the impurity elements S and O from the sintering atmosphere during the sintering process. As a result, main dispersed phase RE2S3 and minor RE2O2S were formed in situ on the sinter skin. The mechanisms for the stimulation of the migration activity and the directional migration of RE atoms were discussed in terms of the thermodynamics stability of Cr3C2, solubility characteristic of Cr in Co and the polarization or ionization of RE atoms.
