Titlebook: Earth Surface Processes and Environmental Changes in East Asia; Records From Lake-ca Kenji Kashiwaya,Ji Shen,Ju Yong Kim Book 2015 Springer

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書目名稱Earth Surface Processes and Environmental Changes in East Asia影響因子(影響力)




書目名稱Earth Surface Processes and Environmental Changes in East Asia影響因子(影響力)學(xué)科排名




書目名稱Earth Surface Processes and Environmental Changes in East Asia網(wǎng)絡(luò)公開度




書目名稱Earth Surface Processes and Environmental Changes in East Asia網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Earth Surface Processes and Environmental Changes in East Asia被引頻次




書目名稱Earth Surface Processes and Environmental Changes in East Asia被引頻次學(xué)科排名




書目名稱Earth Surface Processes and Environmental Changes in East Asia年度引用




書目名稱Earth Surface Processes and Environmental Changes in East Asia年度引用學(xué)科排名




書目名稱Earth Surface Processes and Environmental Changes in East Asia讀者反饋




書目名稱Earth Surface Processes and Environmental Changes in East Asia讀者反饋學(xué)科排名

厚顏無恥

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

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inundate

Palaeoenvironment and Palaeoclimate Evolution of Northeast China: Based on Multi-proxy Analysis of dry, 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

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 ., ., .

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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

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

腐敗

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

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