NDLI: Lacustrine transgressions in the late Cenozoic Ussuri-Khanka depression (Primor’e)

Content Provider	Springer Nature Link
Author	Korotkii, A. M. Grebennikova, T. A. Karaulova, L. P. Belyanina, N. I.
Copyright Year	2007
Abstract	In the Ussuri-Khanka depression of Primorye, the Quaternary alluvial-lacustrine and lacustrine sedimentogenesis progressed under conditions of transgressive accumulation in response to the depression tectonic subsidence and recurrent climatic fluctuations. The alluvial dams and irregular accumulation are proved to have been the leading factors of lakes’ formation within the depression. As is shown, fluctuations of the water level in limnic reservoirs depended on the climatic changes. New data considered in this work confirm the lacustrine genesis of a greater part of the Middle Pleistocene-Holocene sedimentary succession in the Khanka depression. Two transgressive phases, when the water level in the lakes rose by 1.5–2.0 m above the present one, are established for the Subboreal. The general conclusion is that the mesorhythmic structure of the sedimentary succession in the Ussuri-Khanka depression reflects the influence of climatic fluctuations in the Late Cenozoic.
Starting Page	352
Ending Page	365
Page Count	14
File Format	PDF
ISSN	18197140
Journal	Russian Journal of Pacific Geology
Volume Number	1
Issue Number	4
e-ISSN	18197159
Language	English
Publisher	Nauka/Interperiodica
Publisher Date	2007-01-01
Publisher Place	Moscow
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	lacustrine sediment genesis alluvial dams transgressive phases mesorhythms climatic fluctuations lake level Subboreal Ussuri-Khanka depression Primor’e Geology
Content Type	Text
Resource Type	Article
Subject	Geology Geophysics Geochemistry and Petrology Oceanography Paleontology Stratigraphy

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