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• W2923505643 abstract "Pre-existing paleotopography refers to the paleosurface captured during a certain period of the landform formation process that reflects the surface morphology of paleogeography, records the environmental history of paleo-climate, and indicates the life activities of paleoecology (Simon-Coincon et al. in Palaeogeogr Palaeoclimatol Palaeoecol 129(1–2):51–79, 1997; Retallack et al. in Palaeogeogr Palaeoclimatol Palaeoecol 183(3–4):329–354, 2002; Takeuchi et al. in Palaeogeogr Palaeoclimatol Palaeoecol 254(3–4):462–476, 2007; Campani et al. in Earth Planet Sci Lett 337–338:174–185, 2012; Isherwood et al. in Earth Planet Sci Lett 363:88–96, 2013). Reconstructing the surface elevation, relief, and morphology of paleotopography is essential in understanding the vertical range of mountains, exploring the topographic limitations to landform evolution (Phillips et al. in Sediment Geol 232(3–4):98–118, 2010; Pedersen et al. in Geomorphology 223:96–116, 2014; Xiong et al. in Geomorphology 209:18–26, 2014a) and soil erosion (Bergonse and Reis in J Geogr Sci 25(2):196–210, 2015), and relating these to the interplay between geodynamic and earth surface processes (Campani et al. in Earth Planet Sci Lett 337–338:174–185, 2012). The paleotopography underlying loess landform represents the initial surface before the occurrence of the aeolian depositional process. This loess underlying paleotopography serves as an indicator of the paleogeography and erosion base that restrain the evolution of the current landform. This chapter begins by designing an overall method for reconstructing the loess underlying paleotopography in different spatial scales. The macroscale loess underlying paleotopography is then reconstructed by sampling outcrops from a geological map and by applying the spatial interpolation algorithm on these outcrops. The mesoscale loess underlying paleotopography is reconstructed on a basis of the geophysical drillings and prospecting profiles along the highway built by the government. The microscale loess underlying paleotopography is reconstructed by using the EH4 geophysical detector. The quality of the reconstructed macroscale loess underlying paleotopography is assessed by using different spatial interpolation algorithms and outcrop sampling densities. The scale effect of the reconstructed loess underlying paleotopography is then examined to ensure the accuracy of the results. The geomorphology of the pre-Quaternary period is then investigated based on the reconstructed loess underlying paleotopography." @default.
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• W2923505643 date "2019-01-01" @default.
• W2923505643 modified "2023-10-17" @default.
• W2923505643 title "Reconstruction of the Loess Underlying Paleotopography for Loess Landform Inheritance" @default.
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• W2923505643 doi "https://doi.org/10.1007/978-981-13-6404-4_4" @default.
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