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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
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
Variations in geomagnetic field elements for the last 4000 years based on paleomagnetic studies of the bottom sediments of lake aslikul (southwestern bashkiria) considered in this work. Bottom sediment cores of thickness of up to 3.0 m have been taken with a special
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
Variations in geomagnetic field elements for the last 4000 years based on paleomagnetic studies of the bottom sediments of lake aslikul (southwestern bashkiria) considered in this work. Bottom sediment cores of thickness of up to 3.0 m have been taken with a special
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
Geomagnetic secular variation through the last 3500 years as recorded by lake Aslikul sediments from eastern Europe (Russia) from three lake sediment cores from lake Aslikul in the western Pre-Ural region (Russia). Pollen data
Environmental conditions in northwestern Russia during MIS 5 inferred from the pollen stratigraphy in a sediment core from Lake Ladoga-long core. Its upper 13.30 m comprise Holocene and Lateglacial sediments separated from the lower 11.45 m
Особенности фациальной изменчивости нефтеперспективных межсолевых отложений Южной структурной зоны Припятского прогиба deposits of the Southern structural zone of the Pripyat depression, namely, new data on
the genesis
Geomagnetic secular variation through the last 3500 years as recorded by lake Aslikul sediments from eastern Europe (Russia) from three lake sediment cores from lake Aslikul in the western Pre-Ural region (Russia). Pollen data
Страница 2 из 18173
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