Titlebook: Basement Regions; Alain Godard,Jean-Jacques Lagasquie,Yannick Lageat Book 2001 Springer-Verlag Berlin Heidelberg 2001 Geomorphologie.Geomo

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书目名称Basement Regions影响因子(影响力)




书目名称Basement Regions影响因子(影响力)学科排名




书目名称Basement Regions网络公开度




书目名称Basement Regions网络公开度学科排名




书目名称Basement Regions被引频次




书目名称Basement Regions被引频次学科排名




书目名称Basement Regions年度引用




书目名称Basement Regions年度引用学科排名




书目名称Basement Regions读者反馈




书目名称Basement Regions读者反馈学科排名

范例

Hegel’s Conception of Psychologyural or depositional (although such surfaces may also be flat lying), and are sometimes also termed ‘erosion surfaces’. Erosion, in many contexts, is expected to sculpt geological structures and contrasting lithologies (a process described as ‘differential erosion’, which, in basement terrains often

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Planation Surfaces in Basement Terrainsural or depositional (although such surfaces may also be flat lying), and are sometimes also termed ‘erosion surfaces’. Erosion, in many contexts, is expected to sculpt geological structures and contrasting lithologies (a process described as ‘differential erosion’, which, in basement terrains often

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Chemical Weathering, Regolith and Climate in Metamorphic and Igneous Terrainsntecedent chemical alteration can also increase the efficiency of certain mechanical processes (see Chapter 6). Chemical weathering also acts as a prelude to soil development, which in turn, through the interference of vegetation, may profoundly modify the structure and composition of the weathering

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Landscape Development in Tropical Shield Environmentsfact in mind. Owing to the antiquity and rigidity of cratonic lithospheres, the geomorphological characteristics of shield environments will vary according to the style and magnitude of lithospheric deformation. The geomorphic response to tectonic stresses is also variable, and it is usually possibl

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https://doi.org/10.1007/978-94-010-2828-8rope, was reinforced by the experimental work being carried out at the Centre de Geomorphologie in Caen, at the instigation of Jean-Pierre Lautridou and Brigitte Van Vliet-Lanoe, and at the Laboratoire Rhodanien de Geographie in Lyon, under Bernard Etlicher and Pierre Mandier.