1)  150 ka BP
150kaBP
1.
Fluctuations of Main Chemical Elements since 150 ka BP as Indicated in Chagelebulu Stratigraphical Section, Badain Jaran Desert;
巴丹吉林沙漠查格勒布剖面150kaBP以来存在25个由风成沙丘砂与黄土、古土壤、湖相和冲坡积砂土砾石层构成的沉积旋回。
2)  150 ka BP
150 ka BP
1.
Situated at the southeast of the Mu Us Desert, Ordos Plateau, the Milanggouwan stratigraphical section in the Salawusu River Valley keeps a record of 38 sedimentary cycles of alternate evolution of the aeolian dune layers with the fluvio-lacustrine facies and palaeosols since 150 ka BP.
位于鄂尔多斯高原毛乌素沙漠东南边缘的萨拉乌苏河流域的米浪沟湾剖面,记录了150 ka BP以来的38个风成的砂丘砂与河湖相和古土壤交替演化的沉积旋回。
3)  past 150 ka
150ka
4)  since 13 ka BP
13kaBP以来
1.
The sedimentary sequences since 13 ka BP have been established in the Bala lake area, Kahu Co, northern Tibet, through a study of a lacustrine section.
通过对藏北喀湖错把拉湖区湖积剖面的研究,建立了该区13kaBP以来的沉积序列,并将13kaBP以来的气候划分为2个干冷期和2个湿润期。
5)  4.2 ka BP event
4.2ka BP气候事件
6)  128~1.4 ka BP
128~1.4ka BP
参考词条
补充资料:150kA预焙阳极铝电解槽(白银有色金属公司)


150kA预焙阳极铝电解槽(白银有色金属公司)


150kA预焙阳极铝电解槽 (白银有色金属公司)
说明:补充资料仅用于学习参考,请勿用于其它任何用途。