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- W2388658558 abstract "The morphologic units of Ejin Qi can be divided into middle—low mountain, fluvial—pluvial plain, lake basin and aeolian landform by geologic investigation and interpretation of remote sense picture. Landform feature and sediment age dating can distinguish some of the tectonic and climatic events. The second grade terrace of Sogo Nur Lake formed in Pliocene or Early Pleistocene epoch by sporopollen analysis. The terrace between Sogo Nur and Gaxun Nur Lake was formed by tectonic uplift at the end of Early Pleistocene. The age of sediment is 750±60 ka BP. Another obvious tectonic uplift, which formed the alluvial—lacustrine terrace of Heicheng, occurred at the end of Middle Pleistocene or the beginning of Late Pleistocene according to the sediment dating age, 149±60 ka BP. The first grade terrace of Sogo Nur formed mainly of climatic arid and lake shrinking at early—middle period of Holocene. Harsh climate is showed by the dune relics in section of terrace from early to middle Holocene. The climate was humid from 7360±135a BP to 4740±60 a BP, when sediment of Swan Lake terrace deposited. The climate fluctuated violently during the period or middle—late Holocene. A period abundant in rainfall appeared at 1200 a BP." @default.
- W2388658558 created "2016-06-24" @default.
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- W2388658558 date "2006-01-01" @default.
- W2388658558 modified "2023-09-24" @default.
- W2388658558 title "Tectonic and Climatic Events Recorded by Morphologic Units in Ejin Qi, Inner Mongolia" @default.
- W2388658558 hasPublicationYear "2006" @default.
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