Status and Prospects for Quasi-Non-Destructive Analysis of Ancient Artefacts via LA–ICP–MS

Laser ablation inductively coupled plasma mass spectrometry (LA–ICP–MS) combines a low degree of invasiveness (termed quasi-non-destructive) with measurements of concentrations of elements and/or their isotopic compositions in artefacts. The technique has risen to prominence in archaeometric research. Successful applications include the use of trace elements to document the trade of raw glass from Egypt and Mesopotamia to Mycenaean Greece during the Late Bronze Age and the use of Pb isotope ratios to show that a common source of metal was used to mint bronze coins in an ancient Roman city on the Iberian Peninsula during the reigns of Emperors Augustus to Claudius. Prospects for using LA–ICP–MS for elemental mapping (imaging) and for extending the application of isotopic tracing for archaeometry are evaluated.

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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.