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- W2362734982 abstract "The stratotype of the Lalong Formation is located in the Lalong groove of Buduozangbu on north slope in Gangdisi Mount, Tibet(E84° 23.5′、N30°37.5′).It is measured in 2001 by the Regional Geological Surveying Institute, Geological Surveying Academy of Sichuan Province. The Lalong Formation, about 85m thick, consists of poorly-indurated clastic rocks of lakeshore facies, its top and bottom having an unconformity of Type I each. It is middle Pleistocene in age. The Lalong Formation ususlly shows a geomorphologic landscape with relief on the cliff face. Thus, the study of it not noly has a significance in the perfection of the Quaternary stratigraphic system of this area, and in the enrichment of the Quaternary paleogeographic framework of the Qinghai-Tibet Plateau and of the evidence for the analysis and study of environmental change, but also gives an impetus to the farther development of the tourism in West China." @default.
- W2362734982 created "2016-06-24" @default.
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- W2362734982 date "2003-01-01" @default.
- W2362734982 modified "2023-09-23" @default.
- W2362734982 title "ESTABLISHMENT OF THE MIDDLE PLEISTOCENE LALONG FORMATION ON THE NORTHERN SLOPE OF THE GANGDISI MOUNT,TIBET" @default.
- W2362734982 hasPublicationYear "2003" @default.
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