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Sediment transfer at different spatial and temporal scales in the Sichuan Hilly Basin, China: Synthesizing data from multiple approaches and preliminary interpretation in the context of climatic and anthropogenic drivers, core chronology dating and conventional sediment flux monitoring, were synthesized and interpreted
Micrometeorites in lake sediments of volga-ural region of Russia. For investigation chosen core №4 (56.72545° N, 40.60657° E), were sediment sequence not destructed. Core was divided
Climate changes over the last 13500 years based on lake sediments studies (Lake bolshoe Miassovo, South ural, Russia).3 m) cores were collected by special hydraulical core extractor constructed in institute. For core
Climate, glacial and vegetation history of the polar Ural Mountains since c. 27 cal ka bp, inferred from a 54 m long sediment core from Lake Bolshoye Shchuchye was carried out on a 54 m long sediment succession (Co1321) from Lake Bolshoye Shchuchye. The sedimentological
Geochemical Basis of Climate Change Indication in the Holocene Sediments of Lake Bannoe (Southern Urals, Russia) core of lake sediments were considered; the data were obtained by the X-ray fluores-cence (XRF
Geomagnetic field variations in central Europe over the last 12 000 years from Lake Naroch (Belarus) sediments and the along-core time scales were obtained from 14C data and correlation with archaeomagnetic data from
Processes controlling very low sedimentation rates on the continental slope of the Gonone-Orosei canyon system, NE Sardinia—terrestrial and oceanic significance, the sedimentation rates varying from 6–21 cm/103 years in the lower parts of two cores and from 1.5–3 cm
Geomagnetic field variations in central Europe over the last 12 000 years from Lake Naroch (Belarus) sediments and the along-core time scales were obtained from 14C data and correlation with archaeomagnetic data from
Facial characteristics of the Ufimian bituminous sediments. In this paper log data (GR) and core data from a lot of key deposits were considered to receive the scheme
Seismic investigations of lakes sediments as the basis of paleogeographic and paleoclimatic reconstructions, occurs when a multitude of factors overlap. In order to obtain core sediments that allow to get the most
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