首页|Linkage of Mineral Inclusions and Zoning of Magnetite with Fluid Evolution of Hydrothermal Systems:A Case Study of the Fenghuangshan Cu-Fe-Au Skarn Deposit,Eastern China
Linkage of Mineral Inclusions and Zoning of Magnetite with Fluid Evolution of Hydrothermal Systems:A Case Study of the Fenghuangshan Cu-Fe-Au Skarn Deposit,Eastern China
扫码查看
点击上方二维码区域，可以放大扫码查看
原文链接
NETL
NSTL
万方数据
Magnetite from hydrothermal deposits may show compositional zoning with various min-eral inclusions in response to the evolution of hydrothermal fluids.Magnetite from the Fenghuangshan Cu-Fe-Au skarn deposit(eastern China)is a common mineral formed in the earlier stage of skarniza-tion.Magnetite grains have dark gray and light gray zones and contain diverse mineral inclusions.Dark gray zones have higher Si,Ca,Al,and Mg contents than light gray zones.The magnetite matrix from dark gray zones shows superstructure along the[0-11]zone axis in fast Fourier transform pat-terns,different from magnetite in light gray zones with normal structure.Three types of mineral inclu-sions are identified within magnetite:nano-,micron-and submicron-nanometer inclusions.Nanoinclu-sions hosted in dark gray zones are actinolite,diopside,and trace element-rich magnetite,and these are likely formed by growth entrapment during magnetite crystallization at the skarn stage.The chain-width order-disorder intergrowths of diopside nanoinclusion likely indicate fluctuating fluid composi-tions in a lattice scale.Submicron to nanometer inclusions at the boundary between dark gray and light gray zones are quartz,titanite,and Ti-rich magnetite,which were formed via a dissolution and re-precipitation process at the quartz-sulfide stage.Micron-inclusions randomly distributed in both dark and light gray zones include calcite,ankerite,quartz,and chlorite,and these were formed via penetra-tion of fluids at the carbonate stage.Zoned magnetite was formed by fluid replacement,overgrowth,and fluid infilling.Our study highlights the importance of mineral inclusion assemblages,and textural and chemical zonation of magnetite in constraining fluid evolution.
mineral inclusionsmagnetitemineral zoningskarnore-forming processdeposits
State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550081,China
CAS Key Laboratory of Mineralogy and Metallogeny,Guangdong Provincial Key Laboratory of Mineral Physics and Materials,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China
NETL
NSTL
万方数据
