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

apropos

Comparison of Luminescence Dating Methods on Lake Sediments from a Small Catchment: Example from Lals was much larger than the pIRIR. residual signals. Thus, IRSL. and pIRIR. signals were not completely bleached, which we attribute to the short sediment transport distance in this small catchment. Five corrected bulk radiocarbon (.C) ages agreed with the OSL ages, except for two intervals in which

有罪

Calculus

Earth Surface Processes and Environmental Changes in East AsiaRecords From Lake-ca

LATHE

amplitude

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盤旋

"Von Pol zu Pol Ges?nge sich erneun..."thquakes in tectonically active and climatically humid areas. The Tong-hai earthquake of 1970 in Yunnan, China was detected in the combination (density increase and grain size decrease) for the core sediments obtained from Qilu-he. The Kanbun earthquake of 1662 in Lake Biwa catchment was also detect

調(diào)情

Apoptosis

,Einführung und Begleitung im Unternehmen,d that these big-lake periods were associated with relatively colder climates, broadly corresponding to the Marine Isotope Stage (MIS) 6, MIS 2 and the late Holocene. This hypothesis is supported by further high resolution OSL chronology for a sediment core XK from Xingkai Lake. OSL chronology for t

富饒

Abschnitt Die Spaltung der Welt, 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