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- W2068168052 endingPage "1616" @default.
- W2068168052 startingPage "1613" @default.
- W2068168052 abstract "Earning a High Grade Most of the world's copper and molybdenum come from porphyry-type ore deposits in Earth's crust. The metals are deposited either as veins of concentrated metals in fractured rock or in a confined shell, associated with the edges of magma chamber plumes. But it remains unclear why a front of sharp temperature-pressure gradients, which allows the accumulation of high-grade metal deposits, remains stable. Weis et al. (p. 1613 , published online 15 November; see the Perspective by Ingebritsen ) constructed a hydrothermal model of a porphyry-type system given a supply of magmatic fluids with high metal concentrations. The thermodynamic properties of injected volatile fluids and dynamic variations in host rock permeability, driven by injection-induced fracturing, controlled the stability and evolution of the fronts and allowed for the formation of an extensive network of ore veins from within the magmatic chamber." @default.
- W2068168052 created "2016-06-24" @default.
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- W2068168052 date "2012-12-21" @default.
- W2068168052 modified "2023-10-02" @default.
- W2068168052 title "Porphyry-Copper Ore Shells Form at Stable Pressure-Temperature Fronts Within Dynamic Fluid Plumes" @default.
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- W2068168052 doi "https://doi.org/10.1126/science.1225009" @default.
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