Titlebook: Aeolian Grain Transport; The Erosional Enviro Ole E. Barndorff-Nielsen,Brian B. Willetts Conference proceedings 1991 Springer-Verlag Wien 1

aggression

書目名稱Aeolian Grain Transport影響因子(影響力)




書目名稱Aeolian Grain Transport影響因子(影響力)學(xué)科排名




書目名稱Aeolian Grain Transport網(wǎng)絡(luò)公開度




書目名稱Aeolian Grain Transport網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Aeolian Grain Transport被引頻次




書目名稱Aeolian Grain Transport被引頻次學(xué)科排名




書目名稱Aeolian Grain Transport年度引用




書目名稱Aeolian Grain Transport年度引用學(xué)科排名




書目名稱Aeolian Grain Transport讀者反饋




書目名稱Aeolian Grain Transport讀者反饋學(xué)科排名

EVICT

URN

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Controls on aeolian sand sheet formation exemplified by the Lower Triassic of Helgoland,d. Preservation of the aeolian deposits records the overall low-energy of the littoral processes, and early cementation. The aeolian deposits define sedimentary cycles of various thickness, and it is suggested that the cyclicity records Early Triassic orbital climatic forcing.

averse

受辱

legislate

Hormones

Methodische Konzeption der Untersuchung,s is increasing in the same direction. The grain size 400 μm is a threshold: the upper limit of actual, average aeolian deflation..This area, which previously had a positive sediment balance, during the last drought combined with agricultural overuse became an area of sand and dust removal with a negative sediment balance.

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Controllership im internationalen Vergleich. The present rate of coastal retreat is about 1 to 2 m a year. The coastal erosion rates now observed can be used to estimate the rate of intrusion of sand inland from the coast. Measurements with sand traps and by cartographic comparison give an eastward aeolian flux estimated of between 15 and 30 m. a year per m length of foredune.