Environmental Remediation by Crystallization of Solid Solutions

Foreign ions can be incorporated into minerals during mineral growth and mineral–water interactions, resulting in solid phases with substitutional impurities in their structure. These “cocrystallization” processes control the mobility of minor elements in the environment and can be exploited as a remediation strategy to remove toxic metals from polluted waters and in the design of engineered barriers for the retention of metals, radionuclides, and other inorganic wastes generated by industry. The effectiveness of such remediation tools relies on thermodynamic and mechanistic factors that operate at different scales in space and time.

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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.