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- W2363462677 abstract "More than 6 m thick mountain lacustrine deposits composed mainly of grass peat, peat, clay and sand are found around the Tianchi lake swarm in the Ningwu area, Shanxi, by pitting. According to the Ganhai, Tianchi and Pipahai stratigraphic sections, the lacustrine deposits distributed in the mountain lake district may be divided into 12 beds. Sequence stratigraphic study has revealed that the paleolakes represented by the Ganhai Lake evolved from the shallow lake→lakeshore→swamp. 14C dating and ESR dating of the lacustrine deposits give ages of 10950-260 a BP and 9±3-8±1 ka respectively. The results show that the age of the lacustrine deposits in the mountain lakes is Holocene. According to the characteristics of the sedimentary facies and rock association, combined with the isotope dating, sporopollen analysis and microfossil identification, the Holocene lacustrine stratigraphic sequence of mountain lakes has been established for the first time in the area and this sequence of strata is named the Ganhai Formation." @default.
- W2363462677 created "2016-06-24" @default.
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- W2363462677 date "2006-01-01" @default.
- W2363462677 modified "2023-09-23" @default.
- W2363462677 title "Holocene lacustrine deposits in mountain lakes in Ningwu,Shanxi,China and establishment of the Ganhai Formation" @default.
- W2363462677 hasPublicationYear "2006" @default.
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