Luminescence Applications in Ore Geology, Mining, and Industry

Luminescence applications in ore geology, mining, and beneficiation include remote prospecting, ground-based exploration, and radio metric sorting. Remote prospecting for ores with a drone or helicopter- borne luminescent sensing using laser excitation and time-delayed detection is becoming commonplace. Modern ground-based exploration increasingly utilises outlining of luminescing “fugitive calcite” veinlet halos, whose characteristics can rapidly and inexpensively give information on the overall size of a mineralised system and the principal structural controls on ore fluid migration pathways. Diamonds and scheelite have been found and recovered through X-ray luminescent radiometric sorting, while laser-induced luminescence has great potential, especially for sorting diamonds lacking X-ray luminescence, fluorite, spodumene, and rare earth element (REE)–bearing minerals. The luminescence concept is expanded here to include laser-induced breakdown spectroscopy; its fusion with X-ray techniques provides simultaneous information on both the mineralogical and chemical composition of a rock.

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December 2025 --The Variscan Orogeny in Europe – Understanding Supercontinent Formation

The Variscan orogen formed between 380 and 300 million years ago through several accretionary and collisional cycles, culminating with the construction of the Pangea supercontinent. This process occurred via sequential opening and closure of oceanic basins, synchronous detachment of Gondwana derived continental ribbons, and their outboard amalgamation onto the Laurussia margin. The Variscan orogen is rather unique compared with other orogenic belts on Earth: its overthickened and dominantly magmatic crust in the central belt, surprisingly minor mantle involvement in the magmatic and geodynamic processes, coherent and pulsed magmatism along the collision suture, and its complex accretionary history. Because its final product, Pangea, is the youngest and best-understood supercontinent on Earth, the Variscan orogeny offers clues for understanding the mechanisms of supercontinent formation.