morphology
发表于 2025-3-21 16:39:14
书目名称The Sea Floor影响因子(影响力)<br> http://impactfactor.cn/if/?ISSN=BK0919393<br><br> <br><br>书目名称The Sea Floor影响因子(影响力)学科排名<br> http://impactfactor.cn/ifr/?ISSN=BK0919393<br><br> <br><br>书目名称The Sea Floor网络公开度<br> http://impactfactor.cn/at/?ISSN=BK0919393<br><br> <br><br>书目名称The Sea Floor网络公开度学科排名<br> http://impactfactor.cn/atr/?ISSN=BK0919393<br><br> <br><br>书目名称The Sea Floor被引频次<br> http://impactfactor.cn/tc/?ISSN=BK0919393<br><br> <br><br>书目名称The Sea Floor被引频次学科排名<br> http://impactfactor.cn/tcr/?ISSN=BK0919393<br><br> <br><br>书目名称The Sea Floor年度引用<br> http://impactfactor.cn/ii/?ISSN=BK0919393<br><br> <br><br>书目名称The Sea Floor年度引用学科排名<br> http://impactfactor.cn/iir/?ISSN=BK0919393<br><br> <br><br>书目名称The Sea Floor读者反馈<br> http://impactfactor.cn/5y/?ISSN=BK0919393<br><br> <br><br>书目名称The Sea Floor读者反馈学科排名<br> http://impactfactor.cn/5yr/?ISSN=BK0919393<br><br> <br><br>
终端
发表于 2025-3-21 20:50:44
https://doi.org/10.1007/978-3-662-22519-6Coast; Geologie; Ocean; Oceanography; Ozeanographie; Sediment; Sedimentation; Umweltgeologie; environment; en
地牢
发表于 2025-3-22 01:15:27
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Altitude
发表于 2025-3-22 07:00:25
Book 19932nd editionlogy - now usually subsumed under the concept of Plate Tectonics - brought the realization that convection within the Earth is responsible for the origin of today‘s ocean basins and conti nents, and that the grand features of the Earth‘s surface are the product of ongoing large-scale horizontal mot
飓风
发表于 2025-3-22 10:05:08
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Fecal-Impaction
发表于 2025-3-22 14:02:16
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沉着
发表于 2025-3-22 17:39:30
at has recently heated up again. Darwin drew his inspiration from observations on island life made during the voyage of the Beagle (1831-1836), and his work gave strong impetus to the first global oceanographic expedition, the voyage of HMS Challenger (1872- 1876). Ever since, oceanographic research has been 978-3-662-22519-6
推测
发表于 2025-3-22 23:02:50
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老人病学
发表于 2025-3-23 01:47:50
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allergy
发表于 2025-3-23 06:26:25
Carson K. Leung,Fan Jiang,Tik Wai Poon,Paul-Émile Crevierh lateral aus seiner vorher vertikalen Verlaufsrichtung ab, durchzieht die weiter seitlich liegenden Querfortsatzlöcher des Axis und Atlas und umfaßt dann die Articulatio atlantooccipitalis von dorsal. Diese Strecke wird als Pars atlantis bezeichnet. Im hinteren Atlasbogen findet sich eine Delle für