Published September 14, 2024 | Version v1
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Porphyry copper formation driven by water-fluxed crustal anatexis during flat-slab subduction

Description

Supplemtary Data used in the study entitled 'Lamont et al. (2024) Porphyry copper formation driven by water-fluxed crustal anatexis during flat-slab subduction, Nature Geoscience'.

A compilation of geochronology (U–Pb and Ar-Ar and K-Ar) for intrusive and extrusive igneous rocks, mineralization and porphyry copper deposits, and timing of shortening and extension is provided in Supplementary Table S1. Whole rock geochemical data from igneous rocks in Arizona is provided in Supplementary Table 2. A compilation of Nd, Pb and Hf in zircon isotopes, and two-stage model ages from the SW USA and NW Mexico is provided in Supplementary Table S3. Electron-probe microanalysis data for samples TLAZ22-08 and TLAZ22-167 are in Supplementary Table S4. Thermobarometry Results are provided in Supplementary Table S5. In-situ Rb-Sr Geochronology Results are provided in Table S6, whereas U–Th–Pb Monazite Geochronology Results are provided in Supplementary Table S7.  

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Additional details

Funding

Natural Environment Research Council
National Environmental Isotope Facility 2582.1022