aggression 发表于 2025-3-21 17:36:30
书目名称Aeolian Grain Transport影响因子(影响力)<br> http://figure.impactfactor.cn/if/?ISSN=BK0150459<br><br> <br><br>书目名称Aeolian Grain Transport影响因子(影响力)学科排名<br> http://figure.impactfactor.cn/ifr/?ISSN=BK0150459<br><br> <br><br>书目名称Aeolian Grain Transport网络公开度<br> http://figure.impactfactor.cn/at/?ISSN=BK0150459<br><br> <br><br>书目名称Aeolian Grain Transport网络公开度学科排名<br> http://figure.impactfactor.cn/atr/?ISSN=BK0150459<br><br> <br><br>书目名称Aeolian Grain Transport被引频次<br> http://figure.impactfactor.cn/tc/?ISSN=BK0150459<br><br> <br><br>书目名称Aeolian Grain Transport被引频次学科排名<br> http://figure.impactfactor.cn/tcr/?ISSN=BK0150459<br><br> <br><br>书目名称Aeolian Grain Transport年度引用<br> http://figure.impactfactor.cn/ii/?ISSN=BK0150459<br><br> <br><br>书目名称Aeolian Grain Transport年度引用学科排名<br> http://figure.impactfactor.cn/iir/?ISSN=BK0150459<br><br> <br><br>书目名称Aeolian Grain Transport读者反馈<br> http://figure.impactfactor.cn/5y/?ISSN=BK0150459<br><br> <br><br>书目名称Aeolian Grain Transport读者反馈学科排名<br> http://figure.impactfactor.cn/5yr/?ISSN=BK0150459<br><br> <br><br>EVICT 发表于 2025-3-21 21:44:36
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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 发表于 2025-3-22 15:18:48
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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.榨取 发表于 2025-3-23 09:06:18
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.