坪洲

  • 网络Peng Chau
坪洲坪洲
  1. 其中建造坪洲和小榄避风塘及重建白沙湾公众码头的初步可行性报告也已完成。

    Preliminary project feasibility studies for the Peng Chau and Siu Lam typhoon shelters and the reconstruction of the public pier at Pak Sha Wan were completed .

  2. 这一研究成果表明,坪洲组是一盐系地层,大鹏湾盆地在晚白垩世&古近纪时期是一演化程度较高的硫酸盐型蒸发岩盆地。

    This result suggests that the Pingchau Formation is a salt-bearing sequence , and that the Mirs Bay was once a highly saline evaporate basin during the late Cretaceous to Eogene .

  3. 鄂尔多斯盆地石炭系厚0~600m,属潮坪三角洲相。

    The Carboniferous strata , is up to 0 ~ 600 m thick in Ordos basin , are ascribed to the tidal-delta sediments .

  4. 第二阶段(太原组)潮下带、潮坪、三角洲环境交替出现;

    In the second stage ( Taiyuan Age ), sub-tidal , tidal flat and delta occurred alternatively .