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Updated: May 16, 2026

Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
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Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions

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Porphyry-copper ore shells form at stable pressure-temperature fronts within dynamic fluid plumes

P Weis1, T Driesner, C A Heinrich

  • 1Department of Earth Sciences, Eidgenössische Technische Hochschule (ETH) Zurich, 8092 Zürich, Switzerland. weis@erdw.ethz.ch

Science (New York, N.Y.)
|November 20, 2012
PubMed
Summary

Porphyry copper and gold deposits form from magma chamber fluids. Numerical models reveal how fluid dynamics stabilize metal precipitation, controlling ore deposit size, shape, and grade.

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