Heat flow and the Eurasian-African plate boundary in the eastern part of the Azores-Gibraltar fracture zone

Results from geodetic measurements in th

Results from geodetic measurements in the western part of the African–Eurasian plate boundary

✍ L Bastos; J Osório; A Barbeito; G Hein 📂 Article 📅 1998 🏛 Elsevier Science 🌐 English ⚖ 1011 KB

Friction in the preseparation zone and h

Friction in the preseparation zone and heat transfer in the separation zone of a turbulent boundary layer in the flow of heated air in a diffuser with cooled walls

✍ P. N. Romanenko; A. N. Oblivin; L. G. Shelegova 📂 Article 📅 1968 🏛 Springer US 🌐 English ⚖ 239 KB

Effects of leading-edge roughness on flu

Effects of leading-edge roughness on fluid flow and heat transfer in the transitional boundary layer over a flat plate

✍ Mark W. Pinson; Ting Wang 📂 Article 📅 1997 🏛 Elsevier Science 🌐 English ⚖ 940 KB

New data on the present-day active fluid

New data on the present-day active fluid regime of fractured zones of crystalline basement and sedimentary cover in the eastern part of Volga-Ural region

✍ Irina N. Plotnikova 📂 Article 📅 2008 🏛 Springer 🌐 English ⚖ 746 KB

Heat removal of in‐tube viscous flows to

Heat removal of in‐tube viscous flows to air with the assistance of arrays of plate fins Part I: theoretical aspects involving 3‐D, 2‐D and 1‐D models

✍ Campo, Antonio 📂 Article 📅 2000 🏛 Emerald Group Publishing Limited 🌐 English ⚖ 229 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