(GlasgowSymposium British Geomorphological Research Group (BGRG) en Anglais - 1997)

Document title

Some uncertainties in the derivation of rates of denudation from thermochronologic data

published at : Special Issue: Geomorphic processes/landscape evolution

Authors(s) and Affiliation(s)

(1) School of Earth Sciences, Victorian Institute of Earth and Planeetary Sciences, La Trobe Universit, Bundoora, Victoria, AUSTRALIE


Low-temperature thermochronology, such as that provided by apatite fission-track analysis, provides a valuable means of establishing the timing of major denudational events and associated rates of denudation over geological time-scales of 10[6]-10[8] Ma. Care must be taken, however, in deriving denudation rates from the crustal cooling histories documented by thermochronologic techniques, especially in rapidly eroding terrains, since, in such cases, apparent denudation rates derived from thermochronologic data will usually overestimate true rates if the advective effect of denudation is not included



Symposium British Geomorphological Research Group (BGRG), Glasgow , ROYAUME-UNI (04/01/1996)

published at : Earth surface processes and landforms / ISSN 0197-9337 / CODEN ESPLDB

Editor : Wiley, Chichester - ROYAUME-UNI (1981)

Millesime : 1997, vol. 22, no 3 [pp. 239-248]

Bibliographic references : 36 ref.



INIST-CNRS, Cote INIST : 17355

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1997.
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