44th New Mexico Mineral Symposium
November 1 – 4 44th New Mexico Mineral Symposium, Socorro, NM USA.
November 1 – 4 44th New Mexico Mineral Symposium, Socorro, NM USA.
November 8 – 9 Swiss Geoscience Meeting (SGM 2024), Basel, Switzerland
The Botanical Garden of Palermo, Sicily, Italy, will host the Second Italian Workshop on Fluid and Melt Inclusions (IWI 2024), on November 12, 13, and 14, 2024. The event is […]
November 25 – 28 International Conference on Clays in Natural and Engineered Barriers for Radioactive Waste Confinement (Clay Conference) 2024, Hannover, Germany
December 9 - 13 American Geophysical Union Fall Meeting, Washington, D.C. USA
January 26 – 31 49th International Conference and Expo on Advanced Ceramics and Composites (ICACC2025), Daytona Beach, FL USA
Spectrum Conferences cordially invites you to its "3rd International Summit on Gravitation, Astrophysics and Cosmology"(ISGAC2025), the premier International forum for the discussion of the latest developments in the fields of […]
March 23 – 27 American Chemical Society Spring Meeting, San Diego CA USA
The next Geochemistry Group Research in Progress (GGRiP) meeting will take place in Birmingham on the 8-10th of April 2025.
This year's MSG RiP will take place at the University of Liverpool under the stewardship of John Wheeler. MSG welcomes Barrow Award winner Jamie Connolly and keynote speakers Nick Roberts […]
The Geological Association of Canada (GAC®), the Mineralogical Association of Canada (MAC), and the International Association of Hydrogeologists – Canadian National Chapter (IAH-CNC) 2025 annual conference!
The 3rd IAGC International Conference will be held in Cagliari, Italy from 16 − 21 June, 2025. This meeting will include the 18th Water-Rock Interaction Working Group Meeting (WRI-18), the […]
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.