Geological record of fluid flow and seismogenesis along an erosive subducting plate boundary

Fluid flow and heat transfer of carbon n

Fluid flow and heat transfer of carbon nanotubes along a flat plate with Navier slip boundary

✍ Khan, W. A.; Khan, Z. H.; Rahi, M. 📂 Article 📅 2013 🏛 Springer-Verlag 🌐 English ⚖ 588 KB

Unsteady MHD mixed convection flow of a

Unsteady MHD mixed convection flow of a micropolar fluid along an inclined stretching plate

✍ Aurangzaib, ; Kasim, A.R.M.; Mohammad, N.F.; Shafie, Sharidan 📂 Article 📅 2013 🏛 John Wiley and Sons 🌐 English ⚖ 756 KB

Unsteady boundary layer flow of a Casson

Unsteady boundary layer flow of a Casson fluid due to an impulsively started moving flat plate

✍ M. Mustafa; T. Hayat; I. Pop; A. Aziz 📂 Article 📅 2011 🏛 John Wiley and Sons 🌐 English ⚖ 921 KB

## Abstract This paper discusses the unsteady flow and heat transfer of a Casson fluid over a moving flat plate with a parallel free stream. The analytic solutions of the system of nonlinear partial differential equations valid for all times in the whole spatial domain are constructed in the series

Soret and Dufour effects on the flow of

Soret and Dufour effects on the flow of an Erying-Powell fluid over a flat plate with convective boundary condition

✍ Qasim, M. 📂 Article 📅 2014 🏛 Springer-Verlag 🌐 English ⚖ 729 KB

[American Institute of Aeronautics and A

[American Institute of Aeronautics and Astronautics 1st National Fluid Dynamics Conference - Cincinnati,OH,U.S.A. (25 July 1988 - 28 July 1988)] 1st National Fluid Dynamics Conference - Particle injection into an incompressible laminar boundary layer flow along a semi-infinite flat plate

✍ MURAMOTO, KENNETH 📂 Article 📅 1988 🏛 American Institute of Aeronautics and Astronautics ⚖ 567 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