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the claim
Metals are segregated and separated within the Earth's crust
the verdict
SUPPORTED
the evidence backs this
refutedsupported
the weight of evidence
6 sources for · 0 against

Multiple geochemical and geological studies demonstrate that various metals are heterogeneously distributed, segregated, and concentrated within specific domains and depths of the Earth's crust.

Evidence for · 6
2023 · cited by 52
The study maps spatial heterogeneity and segregation of critical metal ore systems (W-Sn, REE, Cu-Au, U, Ag-Pb-Zn) within different crustal domains.
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The analysis

The claim is specific and testable regarding whether metals are segregated within the Earth's crust. The retrieved papers consistently provide geological, isotopic, and geochemical evidence showing that different metals undergo segregation, fractional crystallization, sulfide accumulation, and spatial distribution across various crustal domains and depths. Therefore, the verdict is SUPPORTED.

More for · 5
2018 · cited by 41
It discusses how previous sulfide segregation at depth in the lower arc crust causes PGE depletion, indicating spatial metal separation during magmatic processes.
2024 · cited by 35
It examines lower-crustal processes and pre-enriched crustal sources involved in the genesis of porphyry copper deposits.
2019 · cited by 34
It notes that Cu-Ni sulfide mineralization and segregation occur in specific gabbroic complexes within the crust.
2022 · cited by 5
It discusses how sulfide-fluid associations and segregation processes concentrate metals in ore bodies within sub-volcanic plumbing systems.
2023 · cited by 4
It provides evidence that the continental crust is depleted in copper due to the segregation and accumulation of sulfides during intracrustal differentiation.
Everything we examined (12)
We also searched for evidence AGAINST this claim, not only for it.
  1. Crustal architectural controls on critical metal ore systems in South China based on Hf isotopic mappingpeer-reviewedsupports
  2. Geochronological, Petrological, and Geochemical Studies of the Daxueshan Magmatic Ni-Cu Sulfide Deposit in the Tethyan Orogenic Belt, Southwest Chinapeer-reviewedsupports
  3. Porphyry copper formation driven by water-fluxed crustal melting during flat-slab subductionpeer-reviewedsupports
  4. Geochronology, petrogenesis and tectonic implications of the newly discovered Cu–Ni sulfide-mineralized Yueyawan gabbroic complex, Kalatag district, northwestern Eastern Tianshan, NW Chinapeer-reviewedsupports
  5. Sulfide resorption contributes to porphyry deposit formation in collisional settingspeer-reviewedno side takennot shown: read and judged not to bear on this claim
  6. Plume-subduction interaction forms large auriferous provinces.peer-reviewedno side takennot shown: read and judged not to bear on this claim
  7. From birth to death: The role of upper-crustal thermal maturation and volcanism in porphyry ore formation revealed in the Yerington districtpeer-reviewedno side takennot shown: read and judged not to bear on this claim
  8. Cumulative Anthropogenic Impacts of Past and Future Emissions and Releases on the Global Mercury Cycle.peer-reviewedno side takennot shown: read and judged not to bear on this claim
  9. The critical role of magma degassing in sulphide melt mobility and metal enrichment.peer-reviewedsupports
  10. Sulfur and metal fertilization of the lower continental crust.peer-reviewedno side takennot shown: read and judged not to bear on this claim
  11. Copper isotope evidence for sulfide fractionation and lower crustal foundering in making continental crust.peer-reviewedsupports
  12. Oxidized sediment recycling as a driver for postsubduction porphyry copper formation.peer-reviewedno side takennot shown: read and judged not to bear on this claim
The paper trail · every fact has a biography
first checked06 Aug 2026
judged → SUPPORTED · 8606 Aug 2026
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