To investigate the enrichment processes of Fe in the skarn system, texture and geochemistry of magnetite from the Jinshandian Fe deposit located in eastern China were analyzed. …
WhatsApp: +86 18221755073Here we investigate an ore-forming intrusion associated with a typical iron skarn deposit to explore the magmatic evolution from mineral zoning textures, and to constrain the …
WhatsApp: +86 18221755073U-Pb ages and trace element compositions of two types of hydrothermal titanite from the Jinshandian iron skarn deposit, southeastern Hubei Province, have been successfully …
WhatsApp: +86 18221755073In this study, we present a comparative study between a newly identified subsurface IOA ore body located at the apex of a diorite porphyry and the iron skarn ore bodies located …
WhatsApp: +86 18221755073Composition Analysis of Jinshandian Iron Ore Mineralogical and sulfur isotopic evidence for · Both these values are markedly heavier than the common δ 34 S values of sulfides from magmatic …
WhatsApp: +86 18221755073U-Pb ages and trace element compositions of two types of hydrothermal titanite from the Jinshandian iron skarn deposit, southeastern Hubei Province, have been successfully analyzed by...
WhatsApp: +86 18221755073In this study, we examine detailed textural relationships and halogen signatures of scapolites formed at different paragenetic stages, together with B isotope analysis of …
WhatsApp: +86 18221755073In this study, we present a comparative study between a newly identified subsurface IOA ore body located at the apex of a diorite porphyry and the iron skarn ore bodies located …
WhatsApp: +86 18221755073Jinshandian (Edong district, eastern China) is an iron skarn formed by the intense interplay between magmatic-hydrothermal fluids and evaporite-bearing wall rocks.
WhatsApp: +86 18221755073In this paper, we present new U–Pb geochronological data for magmatic zircon and hydrothermal titanite, as well as 40 Ar/ 39 Ar ages on hydrothermal phlogopite, to determine …
WhatsApp: +86 18221755073Jinshandian (Edong district, eastern China) is an iron skarn formed by the intense interplay between magmatic-hydrothermal fluids and evaporite-bearing wall rocks.
WhatsApp: +86 18221755073To investigate the enrichment processes of Fe in the skarn system, texture and geochemistry of magnetite from the Jinshandian Fe deposit located in eastern China were analyzed. …
WhatsApp: +86 18221755073In this study, we present detailed textures and geochemical compositions of newly identified colloform pyrite (Py1) and late coarse-grained pyrite (Py2) from the Jinshandian iron …
WhatsApp: +86 18221755073In this paper, we present new U–Pb geochronological data for magmatic zircon and hydrothermal titanite, as well as 40 Ar/ 39 Ar ages on hydrothermal phlogopite, to determine …
WhatsApp: +86 18221755073plants in the public sector, India's consumption of iron ore will increase considerably. The prices paid to the mine owners for the ore are directly linked with the contents of iron, phosphorus, …
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