Combining Metal Stable Isotope Fractionation Theory with Experiments

Theoretical, experimental, and empirical methods for estimating isotope fractionations often complement one another in precision and ease of application. In metal isotope systems, a combined approach to calibrating stable isotope fractionation shows great promise, but it is sometimes necessary to resolve significant disagreements between theoretical models and empirical data. Here we introduce some of the principles and techniques used to estimate metal isotope signatures in low-temperature environments, and we highlight potential sources of uncertainty and error. We also discuss strategies for integrating theoretical calculations with data from laboratory experiments and natural sample suites.

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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.