Natural Zeolites: Pathways to Green and Durable Cement and Concrete

Rocks containing natural zeolites have been used since antiquity as components of concrete and mortars. As pozzolans, natural zeolites react with slaked lime (Ca(OH)2) or Portland cement and water to form sparingly soluble calcium silicate and calcium aluminate hydrates. This pozzolanic reaction improves the long-term strength and durability of the mortar and concrete. Moreover, natural zeolites may replace Portland cement, reducing CO2 emissions from cement production, thereby making them an interesting decarbonization solution. Ongoing mineralogical investigations have revealed the influence of zeolitic framework topology, Si/Al ratio, and cation-exchange capacity on the pozzolanic reactivity of natural zeolites within cementitious matrices. This research paves the way to better utilization of this natural resource and leveraging its CO2-saving potential in construction.

This content is for Registered members only. To subscribe, please
join one of our participating societies or contact the Editorial Team.

Login
Already a member? Log in here
Scroll to Top

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.