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

corrupt

書目名稱Basement Regions影響因子(影響力)




書目名稱Basement Regions影響因子(影響力)學科排名




書目名稱Basement Regions網(wǎng)絡(luò)公開度




書目名稱Basement Regions網(wǎng)絡(luò)公開度學科排名




書目名稱Basement Regions被引頻次




書目名稱Basement Regions被引頻次學科排名




書目名稱Basement Regions年度引用




書目名稱Basement Regions年度引用學科排名




書目名稱Basement Regions讀者反饋




書目名稱Basement Regions讀者反饋學科排名

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

figment

糾纏,纏繞

Enrage

放肆的你

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

Isometric

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

cogent

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

富足女人

breadth

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.