Some isostatic and thermal consequences of the vertical strain geometry in convergent orogens
- 22 October 2002
- journal article
- Published by Elsevier
- Vol. 98 (2) , 154-165
- https://doi.org/10.1016/0012-821x(90)90056-4
Abstract
No abstract availableKeywords
This publication has 13 references indexed in Scilit:
- A model for low‐pressure facies metamorphism during crustal thickeningJournal of Metamorphic Geology, 1990
- Secular trends in the thermal evolution of metamorphic terrainsEarth and Planetary Science Letters, 1989
- Horizontal structures in granulite terrains: A record of mountain building or mountain collapse?Geology, 1989
- The mechanics of the Tibetan PlateauPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1988
- Finite strain calculations of continental deformation: 1. Method and general results for convergent zonesJournal of Geophysical Research, 1986
- Pressure--Temperature--Time Paths of Regional Metamorphism I. Heat Transfer during the Evolution of Regions of Thickened Continental CrustJournal of Petrology, 1984
- Coesite and pure pyrope in high-grade blueschists of the Western Alps: a first record and some consequencesContributions to Mineralogy and Petrology, 1984
- Mechanisms of crustal deformationJournal of the Geological Society, 1983
- A thin viscous sheet model for continental deformationGeophysical Journal International, 1982
- Some remarks on the development of sedimentary basinsEarth and Planetary Science Letters, 1978