Definition
The use of thermochronometers having closure temperatures less than 200 °C that allow evaluation of the timing of geomorphic events or rates of landscape change caused by processes such as uplift, incision, exhumation, erosion, transport, and sedimentation.
Introduction
Continental topography links to some of the most fundamental questions about earth processes and history. Some modern topographic features, such as the Altiplano, Himalaya, or Tarim basin, are among the most striking physical features on the planet. Understanding the timing and processes that created these topographic spectacles would seemly provide profound insight into planetary dynamics. Topography is also central to interactions between a wide range of phenomena, including mantle circulation (e.g., Cazenave et al., 1989; Forte et al., 1993), ocean chemical evolution (e.g., Raymo et al., 1988), biota and biotic evolution (e.g., Dietrich and Perron, 2006), and weather and climate on both local and global...
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Simon-Labric, T. (2015). Thermochronology, Landform Evolution. In: Jack Rink, W., Thompson, J.W. (eds) Encyclopedia of Scientific Dating Methods. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-6304-3_190
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DOI: https://doi.org/10.1007/978-94-007-6304-3_190
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