Triple oxygen isotope compositions of iron oxide-apatite deposits – a window into ore formation processes and the ancient atmosphere ...
Iron oxide - apatite (IOA) deposits are magnetite- and apatite-rich rock assemblages that are hosted by intermediate to felsic magmatic rocks, and are frequently mined for iron. The geological formation mechanisms of IOA deposits were suggested to involve either high-temperature silicate, iron oxide...
| Main Authors: | , , , , , , , |
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| Format: | Text |
| Language: | English |
| Published: |
Deutsche Geologische Gesellschaft - Geologische Vereinigung e.V. (DGGV)
2022
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| Subjects: | |
| Online Access: | https://dx.doi.org/10.48380/231w-1v53 https://www.dggv.de/e-publikationen/triple-oxygen-isotope-compositions-of-iron-oxide-apatite-deposits-a-window-into-ore-formation-processes-and-the-ancient-atmosphere |
| Summary: | Iron oxide - apatite (IOA) deposits are magnetite- and apatite-rich rock assemblages that are hosted by intermediate to felsic magmatic rocks, and are frequently mined for iron. The geological formation mechanisms of IOA deposits were suggested to involve either high-temperature silicate, iron oxide and/or sulfate melts or, alternatively, hydrothermal processes at more moderate temperatures. Here, we show that magnetite and apatite samples from the type locality of the deposits in the Kiruna district, northern Sweden, contain up to tens of atom percent oxygen from evaporitic sulfate, as is demonstrated by their anomalously low Δ′17O values. In order to explain this observation in conjunction with field evidence for an igneous origin of the deposits from Kiruna, we propose that the IOA assemblage of Kiruna crystallised from iron-rich sulfate melts and/or from sulfate-rich iron oxide melts. The iron-rich sulfate melts would have formed when evaporite-rich sediments melted by anatexis and scavenged iron from ... |
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