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- W4248851866 abstract "上新世盐类沉积仅分布于柴达木盆地两部、昆仑山和唐古拉山北坡;晚更新世-全新世盐类沉积广布于羌塘和柴达木盆地。盐湖沉积只有蒸发岩和碎屑沉积物互层特点, 系干湿交替的内陆气候和动荡浅水环境下的湖相沉积。迄今已发现62种盐类矿物, 其析出具有阶段性特征, 青藏更新世-全新世盐湖自析阶段的起始时间分别为<sup>14</sup>C 24000和9000a B.P., 钾盐和硼酸盐各有两种典型的矿物共生组合。丰富的盐湖矿物资源是该区走向繁荣的物质基础之一。;Saline deposits in Pliocene distribute in the Western Qaidam Basin, the Kunlun Mountains' and the Northern Tanggola Range, but those in Late Pleistocene-Holocene Epoch widely distribute in Northern Xizang and the Qaidam Basin. Salt lake deposits arc characterized by interbeded evaporatic and clastic sediments with lacustrine facies deposits under inland, dry/wet alternating climatic and unstable shallow water circumstances. 62 saline minerals have been discovered as of now. There exist several separation stages. The beginning age of the self-separation:stage of salt lakes of Late-Pleistocene-Holocene Epoch in the Qinghai-Xizang Plateau arc 24000 a B.P.and 9000 a B.P. respectively according to <sup>l4</sup>C dating. Potash salt and borate have two typical mineral assemblages respectively. Abundance of mineral resources of salt lake is one of the material bases for the development of this district." @default.
- W4248851866 created "2022-05-12" @default.
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- W4248851866 date "1991-01-01" @default.
- W4248851866 modified "2023-09-25" @default.
- W4248851866 title "Saline Deposits And Minerals Of Salt Lakes In Qinghai-Xizang Plateau" @default.
- W4248851866 doi "https://doi.org/10.18307/1991.0101" @default.
- W4248851866 hasPublicationYear "1991" @default.
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