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 […]
August 30 -September 2 16th Quadrennial IAGOD Symposium, Porto, Portugal
October 11 – 14 Geological Society of American Annual Meeting, Denver CO USA
November 6 – 8 46th New Mexico Mineral Symposium, Socorro, NM USA
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.
