Natural Zeolite Crystal Chemistry: Structural Diversity and Behavior Under Non-ambient Conditions

Zeolites have remarkable structural and chemical versatility, arising from their wide range of framework configurations, the variable populations of extra-framework species occupying their structural voids, and their ability to adsorb molecular species. These characteristics underpin unique properties like cation exchange, molecular sieving, selective adsorption, and catalytic behavior. Their framework flexibility allows dynamic responses to environmental stimuli, including temperature, pressure, and relative humidity, leading to phenomena such as negative thermal expansion (contraction), amorphization, and dehydration. Under pressure, zeolites can undergo pressure-induced incorporation of ions and molecules from surrounding fluids, modifying their structure and properties. Understanding these responses opens new pathways for tailoring zeolite behavior for technological applications and deepening our comprehension of their role in geological processes.

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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.