The low plain became an ext ensive sand sea environment under the actions of the cold and dry winter monsoon , the sand sea environment was called the shelf sand sea and constituted the eas t margin of the North Hemisphere desert belt.
英
美
- 該低平原在寒冷而又干燥的冬季風(fēng)作用之下 ,出現了大面積的沙海環(huán)境 ,或者稱(chēng)為陸架沙海 ,并構成北半球沙漠帶的最東緣