2025 Goldschmidt Conference
July 6 – 11 2025 Goldschmidt Conference, Prague, Czech Republic
July 6 – 11 2025 Goldschmidt Conference, Prague, Czech Republic
July 13 – 18 AIPEA International Clay Conference, Dublin, Ireland.
The theme of the conference is ‘Sustaining Clays’ to emphasise the myriad roles played by clays, clay minerals, and the closely allied layered double hydroxides and natural zeolites in sustainable development, the use and management of very many resources, and their bright future in tomorrow’s world. Our key aim with this conference is to integrate […]
July 14 – 18 88th Annual Meeting of the Meteoritical Society, Perth, Australia
July 18 - 23 75th American Crystallographic Association Annual Meeting, Lombard, IL USA
July 20 – 25 Materials Challenges in Alternative & Renewable Energy 2025 (MCARE 2025) combined with the 6th Annual Energy Harvesting Society Meeting (EHS 2025), Bellevue, WA USA
Spectrum Conferences invites you to prestigious event 2nd International Summit on Applied Science, Engineering and Technology. A premier conference focusing on the latest developments and modern trends in Applied Science, Engineering and Technology is going to be held in Frankfurt, Germany during July 21-23, 2025.
August 17 – 21 American Chemical Society Fall Meeting, Washington DC USA
October 19 – 22 Geological Society of American Annual Meeting, San Antonio, TX USA
November 7 – 9 45th New Mexico Mineral Symposium, Socorro, NM USA
March 22 – 26 American Chemical Society Spring Meeting, Atlanta GA USA
This conference covers everything to do with clay minerals--in geology, soil science, technology, and the origins of life. This particular meeting will have a particularly strong focus on natural nanotubes such as halloysite, and will include a field trip to some halloysite mines.
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.