Lyell Collection
Geological Society, London, Special Publications
Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help

Keywords:
Author:
Advanced search>>
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Grujic, D.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation
Geological Society, London, Special Publications; 2006; v. 268; p. 25-37;
DOI: 10.1144/GSL.SP.2006.268.01.02
© 2006 Geological Society of London

Introduction

Channel flow and continental collision tectonics: an overview

D. Grujic

Department of Earth Sciences, Dalhousie University, Halifax, Canada dgrujic{at}dal.ca

The principle of channel flow as defined in fluid dynamics has been used in continental geodynamics since the 1980s. The basic equations for one-dimensional flow introduced to geologists by Turcotte and Schubert were further developed by several research groups to meet the needs of specific studies. The most substantive differences among numerical models are results of different solutions for flow in crust, developed for different boundary conditions. The concept of channel flow has met with strong opposition and criticism from geophysicists and modellers. Although it is difficult to prove unambiguously that there is an active weak channel, it is still the most successful model to explain and predict the tectonics, metamorphism and exhumation of high-grade terranes in some orogens. Moreover, the concept of channel flow has stimulated novel approaches to the study of both the tectonics and metamorphism of large, hot orogens and the interaction between tectonic and surface processes.





This article has been cited by other articles:


Home page
 Journal of the Geological SocietyHome page
N. Harris
Channel flow and the Himalayan-Tibetan orogen: a critical review
Journal of the Geological Society, 2007; 164: 511 - 523.
[Abstract] [Full Text] [PDF]

Home page
 Geological Society, London, Special PublicationsHome page
L. Godin, D. Grujic, R. D. Law, and M. P. Searle
Channel flow, ductile extrusion and exhumation in continental collision zones: an introduction
Geological Society, London, Special Publications, 2006; 268: 1 - 23.
[Abstract] [PDF]

Home page
 Geological Society, London, Special PublicationsHome page
M. J. Jessup, R. D. Law, M. P. Searle, and M. S. Hubbard
Structural evolution and vorticity of flow during extrusion and exhumation of the Greater Himalayan Slab, Mount Everest Massif, Tibet/Nepal: implications for orogen-scale flow partitioning
Geological Society, London, Special Publications, 2006; 268: 379 - 413.
[Abstract] [PDF]