On the growth and collapse of wide orogenic belts
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/118/1/255/1569206/118-1-255.pdf
Reference47 articles.
1. Structure and evolution of the Himalaya-Tibet orogenic belt;Allègre;Nature,1984
2. A field study of Pleistocene rifts in Tibet;Armijo;EOS Trans. Am. geophys. Un.,1982
3. Quaternary extension of Southern Tibet: field observations and tectonic implications;Armijo;J. geophys. Res.,1986
4. Stresses in the lithosphere caused by crustal thickness inhomogeneities;Artyushkov;J. geophys. Res.,1973
5. Stress distribution associated with compensated plateau uplift structures with application to continental splitting mechanism;Bott;Geophys. J. R. astr. Soc.,1979
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1. The Moho as a transition zone: A revisit from seismic and electrical properties of minerals and rocks;Tectonophysics;2013-12
2. Lithospheric scale gravitational flow: the impact of body forces on orogenic processes from Archaean to Phanerozoic;Geological Society, London, Special Publications;2006
3. The Fluid-absent Partial Melting of a Zoisite-bearing Quartz Eclogite from 1middle dot0 to 3middle dot2 GPa; Implications for Melting in Thickened Continental Crust and for Subduction-zone Processes;Journal of Petrology;2002-02-01
4. From lithospheric thickening and divergent collapse to active continental rifting;Geological Society, London, Special Publications;2001
5. Rayleigh-Taylor instabilities of a self-gravitating Earth;Journal of Geodynamics;1995-11
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