磨损
发表于 2025-3-21 17:54:31
书目名称Earth Surface Processes and Environmental Changes in East Asia影响因子(影响力)<br> http://figure.impactfactor.cn/if/?ISSN=BK0300858<br><br> <br><br>书目名称Earth Surface Processes and Environmental Changes in East Asia影响因子(影响力)学科排名<br> http://figure.impactfactor.cn/ifr/?ISSN=BK0300858<br><br> <br><br>书目名称Earth Surface Processes and Environmental Changes in East Asia网络公开度<br> http://figure.impactfactor.cn/at/?ISSN=BK0300858<br><br> <br><br>书目名称Earth Surface Processes and Environmental Changes in East Asia网络公开度学科排名<br> http://figure.impactfactor.cn/atr/?ISSN=BK0300858<br><br> <br><br>书目名称Earth Surface Processes and Environmental Changes in East Asia被引频次<br> http://figure.impactfactor.cn/tc/?ISSN=BK0300858<br><br> <br><br>书目名称Earth Surface Processes and Environmental Changes in East Asia被引频次学科排名<br> http://figure.impactfactor.cn/tcr/?ISSN=BK0300858<br><br> <br><br>书目名称Earth Surface Processes and Environmental Changes in East Asia年度引用<br> http://figure.impactfactor.cn/ii/?ISSN=BK0300858<br><br> <br><br>书目名称Earth Surface Processes and Environmental Changes in East Asia年度引用学科排名<br> http://figure.impactfactor.cn/iir/?ISSN=BK0300858<br><br> <br><br>书目名称Earth Surface Processes and Environmental Changes in East Asia读者反馈<br> http://figure.impactfactor.cn/5y/?ISSN=BK0300858<br><br> <br><br>书目名称Earth Surface Processes and Environmental Changes in East Asia读者反馈学科排名<br> http://figure.impactfactor.cn/5yr/?ISSN=BK0300858<br><br> <br><br>
厚颜无耻
发表于 2025-3-21 23:01:21
Centennial-Scale Environmental Changes in Terhiin Tsagaan Lake, Mongolia Inferred from Lacustrine Se, can be used for the indicator for some hydro-climatic events and/or lake level changes. The gradual fluctuation of the averaged brightness was well correlated with the contents of biogenic silica plus organic matter. The profiles of the brightness can provide high resolution information regarding
投票
发表于 2025-3-22 02:54:50
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inundate
发表于 2025-3-22 08:01:16
Palaeoenvironment and Palaeoclimate Evolution of Northeast China: Based on Multi-proxy Analysis ofdry, and this period corresponded to the LGM (Last Glacial Maximum). During the period between 19,940 and 14,510 cal a BP, the precipitation increased compared to the previous period and temperature also increased to some extent. During the period between 14,510 and 11,500 cal a BP, the late glacia
aviator
发表于 2025-3-22 12:21:27
Paleovegetation and Paleoclimate Evolution of Past 27.7 cal ka BP Recorded by Pollen and Charcoal o climate condition. From 19.9 to 14.5 cal ka BP, there was broad-leaved forest steppe with . and . as the main component when . and Ferns increased greatly, which suggested a cold-wet climatic trend. During 14.5 ∼ 10.8 cal ka BP, the study region was occupied by sparse forest grassland with ., ., .
的事物
发表于 2025-3-22 13:43:17
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的事物
发表于 2025-3-22 20:47:14
Rapid Environmental Change of Jingpo Lake in Mid-Holocene: Inferred from Fluvial/Lacustrine Sedimen yr BP); (iii) Unite 3, lacustrine sedimentary facies (above 1,154 cm, after ∼5,060 cal. yr BP). Our results suggest that Unite 1 represents fluvial sedimentary facies, while the lacustrine sedimentary facies developed afterwards. Between 1,250 and 1,240 cm intervals, the highest MS values and high
Loathe
发表于 2025-3-22 22:04:12
Palaeohydrological and Palaeoenvironmental Fluctuations of the Historic Eurimji Lake,ost artificial layers in Lake Eurimji, which vertically constitute the bottom of Eurimji bank or dyke at about 306.5 m.a.s.l. The height is about 15 m. The present study reconstructs the paleo-precipitation of Lake Eurimji by applying an age mode to core sediments in the ER3-1 borehole using the mea
腐败
发表于 2025-3-23 05:16:59
Late Quaternary Environmental Changes of the Hwajinpo and Songjiho Lagoons on the Eastern Coast of . Although the lithologic changes in the both lagoons do not show any temporal similarity, T-R (transgression and regression) trends based on the grain size variation shows simultaneity. T-R diagram presents three cycles clearly since 7,800 .C yr BP. Highstand sea levels (transgressions) are appeare
石墨
发表于 2025-3-23 09:16:42
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