Luminescence Images: What is it That You See?

Luminescence imaging and hyperspectral luminescence mapping are powerful analytical tools with widespread applications in geosciences and materials science. The luminescence of minerals is mainly a defect phenomenon caused by lattice defects and/or impurity elements. This in turn allows one to study trace-element composition and the structural state of a sample by means of its emission. One of the most spectacular and widely used applications of luminescence images is to visualise internal textures in minerals that are not revealed by other analytical techniques. Herein we present a selection of examples for the extraordinary sensitivity of luminescence imaging. We also show that precise information on samples is obtained if luminescence imaging is combined with spectroscopic analysis of the emission and/ or complementary analytical techniques.

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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.