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Oxygen isotopes trace the origins of Earth’s earliest continental crust

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  1. Article

    Open Access

    Zinc on the edge—isotopic and geophysical evidence that cratonic edges control world-class shale-hosted zinc-lead deposits

    The North Australian Zinc Belt is the largest zinc-lead province in the world, containing three of the ten largest known individual deposits (HYC, Hilton-George Fisher, and Mount Isa). The Northern Cordillera ...

    David L. Huston, David C. Champion, Karol Czarnota, **gming Duan in Mineralium Deposita (2023)

  2. Chapter

    Applications of Lead Isotopes to Ore Geology, Metallogenesis and Exploration

    Although lead isotopes are most commonly used to date geological events, including mineralizing events, they also can provide information on many aspects of metallogeny and can be directly used in mineral expl...

    David L. Huston, David C. Champion in Isotopes in Economic Geology, Metallogenes… (2023)

  3. Chapter

    Applications of Neodymium Isotopes to Ore Deposits and Metallogenic Terranes; Using Regional Isotopic Maps and the Mineral Systems Concept

    Although radiogenic isotopes historically have been used in ore genesis studies for age dating and as tracers, here we document the use of regional- and continental-scale Sm–Nd isotope data and derived isotopi...

    David C. Champion, David L. Huston in Isotopes in Economic Geology, Metallogenes… (2023)

  4. Article

    Open Access

    Lithospheric conductors reveal source regions of convergent margin mineral systems

    The clean energy transition will require a vast increase in metal supply, yet new mineral deposit discoveries are declining, due in part to challenges associated with exploring under sedimentary and volcanic c...

    Alison Kirkby, Karol Czarnota, David L. Huston, David C. Champion in Scientific Reports (2022)

  5. Article

    Open Access

    No evidence for high-pressure melting of Earth’s crust in the Archean

    Much of the present-day volume of Earth’s continental crust had formed by the end of the Archean Eon, 2.5 billion years ago, through the conversion of basaltic (mafic) crust into sodic granite of tonalite, tro...

    Robert H. Smithies, Yongjun Lu, Tim E. Johnson in Nature Communications (2019)