Evolution of passive margin escarpments: What can we learn from low‐temperature thermochronology?
- 21 December 2004
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Earth Surface
- Vol. 109 (F4)
- https://doi.org/10.1029/2004jf000147
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- Pecube: a new finite-element code to solve the 3D heat transport equation including the effects of a time-varying, finite amplitude surface topographyComputers & Geosciences, 2003
- Denudational history along a transect across the Drakensberg Escarpment of southern Africa derived from apatite fission track thermochronologyJournal of Geophysical Research, 2002
- Estimating exhumation rate and relief evolution by spectral analysis of age–elevation datasetsTerra Nova, 2002
- Quantifying the effect of recent relief changes on age–elevation relationshipsPublished by Elsevier ,2002
- Quantifying passive margin denudation and landscape development using a combined fission-track thermochronology and cosmogenic isotope analysis approachEarth and Planetary Science Letters, 2000
- Denudation rates for the southern Drakensberg escarpment, SE Africa, derived from in-situ- produced cosmogenic 36 C1: initial resultsJournal of the Geological Society, 1999
- The tectonic history of the Tasman Sea: A puzzle with 13 piecesJournal of Geophysical Research, 1998
- Modelling landscape evolution on geological time scales: a new method based on irregular spatial discretizationBasin Research, 1997
- Constraining variability in south-east Australian long-term denudation rates using a combined geomorphological and thermochronological approachZeitschrift für Geomorphologie, 1992
- Conduction of Heat in SolidsPhysics Today, 1962