Hornblendite in the Lower Crust: A Possible Source for Porphyry Cu Deposits
Abstract Lower crustal sulfide‐bearing Cu‐rich cumulates, mainly occurring as hornblendite, have been proposed as a critical source component for the development of giant porphyry Cu deposits (PCDs); however, their mineralogical and geochemical nature remain elusive. We present integrated geochemica...
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| Autors principals: | , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Wiley
2026-05-01
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| Col·lecció: | Geochemistry, Geophysics, Geosystems |
| Matèries: | |
| Accés en línia: | https://doi.org/10.1029/2025GC012870 |
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