Telescoping of isotherms beneath the South Tibetan Detachment, Mount Everest Massif: implications for magnitude of internal flow during extrusi on of the Greater Himalayan Slab

Authors

  • Richard D Law Department of Geosciences, Virginia Tech, Blacksburg, VA24061, USA
  • Micah J Jessup Department of Earth & Planetary Sciences, University of Tennessee, Knoxville, TN 37969, USA
  • Michael P Searle Department of Earth Sciences, University of Oxford, Oxford OX1 3PR, UK
  • John M Cottle Department of Earth Sciences, University of Oxford, Oxford OX1 3PR, UK
  • David Waters Department of Earth & Planetary Sciences, University of Tennessee, Knoxville, TN 37969, USA

DOI:

https://doi.org/10.3126/hjs.v5i7.1281

Abstract

DOI = 10.3126/hjs.v5i7.1281

Himalayan Journal of Sciences Vol.5(7) (Special Issue) 2008 p.86-87

Downloads

Download data is not yet available.
Abstract
615
PDF
543

Downloads

How to Cite

Law, R. D., Jessup, M. J., Searle, M. P., Cottle, J. M., & Waters, D. (2008). Telescoping of isotherms beneath the South Tibetan Detachment, Mount Everest Massif: implications for magnitude of internal flow during extrusi on of the Greater Himalayan Slab. Himalayan Journal of Sciences, 5(7), 86–87. https://doi.org/10.3126/hjs.v5i7.1281

Issue

Vol. 5 No. 7 (2008)

Section

Extended Abstracts