Crust/Mantle Recycling at Convergence Zones || From Plate Tectonics to Global Domain Tectonics

Crust/Mantle Recycling at Convergence Zo

Crust/Mantle Recycling at Convergence Zones || A Review of the Thermal-Mechanical Structures at Convergent Plate Boundaries and their Implications for Crust/Mantle Recycling

✍ Hart, Stanley R.; Gülen, Levent 📂 Article 📅 1989 🏛 Springer Netherlands ⚖ 595 KB

Crust/Mantle Recycling at Convergence Zo

Crust/Mantle Recycling at Convergence Zones || Sediment Recycling at Convergent Margins: Constraints from the Cosmogenic Isotope 10Be

✍ Hart, Stanley R.; Gülen, Levent 📂 Article 📅 1989 🏛 Springer Netherlands ⚖ 835 KB

Crust/Mantle Recycling at Convergence Zo

Crust/Mantle Recycling at Convergence Zones || Convection and Gravity Close to Subduction in a Two Layer Mantle: A 3-D Modelisation

✍ Hart, Stanley R.; Gülen, Levent 📂 Article 📅 1989 🏛 Springer Netherlands ⚖ 545 KB

Crust/Mantle Recycling at Convergence Zo

Crust/Mantle Recycling at Convergence Zones || Use of Multispace Technique to Determine the Contribution of Reinjected Sediments in the Mantle (E.G. Lesser Antilles)

✍ Hart, Stanley R.; Gülen, Levent 📂 Article 📅 1989 🏛 Springer Netherlands ⚖ 559 KB

The global network of plate boundaries c

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid-plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains.

✍ L.-E. Ricou 📂 Article 📅 1998 🏛 John Wiley and Sons 🌐 English ⚖ 197 KB

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a sin