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foreland

英 [ˈfɔːlənd]

美 [ˈfɔːrlənd]

n.  前陆; 前沿地; 前方地; 岬; 陆岬

IELTSTEM8

BNC.49474

牛津词典

    noun

    • 前陆;前沿地;前方地
      an area of land which lies in front of sth
      1. 岬;陆岬
        an area of land which sticks out into the sea

        英英释义

        noun

        • land forming the forward margin of something
          1. a natural elevation (especially a rocky one that juts out into the sea)
              Synonym:promontoryheadlandhead

            双语例句

            • Most of the buildings and highways are distributed nearby the Chengshan Town and the foreland.
              增加的建设及交通用地主要集中在月湖以西的成山镇附近和以东的沿海地区。
            • From the Cretaceous, Tarim basin began the new evolutional stage of foreland basin.
              从白垩纪初期开始,塔里木盆地进入晚期前陆盆地演化阶段。
            • Detailed sedimentary research indicates that Late Jurassic Mohe basin contains the alluvial fan, fan-delta and lacustrine facies, belonging to continental molasse deposits of the foreland basin.
              详细的沉积学研究表明:晚侏罗世漠河盆地主要发育冲积扇、扇三角洲和湖泊相沉积,属于前陆盆地的陆相磨拉石部分。
            • The Chuxiong Basin is a typical foreland basin formed in the Mesozoic.
              楚雄盆地为中生代形成的典型前陆盆地。
            • Generally, the basin is a superimposed basin formed by foreland depression of the Late Paleozoic in the lower, and the piedmont depression of the Meso-Cenozoic in the upper.
              它是由晚古生代前陆坳陷和中新生代山前拗陷迭加而成的复合型盆地。
            • The Indosinian foreland fold and thrust belt bordering Yunnan and Guangxi supported further evidence to the Paleotethysides.
              滇桂交界处的印支期前陆褶皱冲断带为古特提斯造山带提供了进一步的证据。
            • Tectonic evolution characteristics of the foreland basin on the southern margin of the Dabie-Sulu orogenic belt;
              大别山东南缘前陆盆地经历了由海相海陆过渡相陆相的演化历程,具有复合叠合盆地特征。
            • According to dynamic characteristics, it can also be divided into single foreland, double forelands and strike-slip foreland basins.
              按其动力学性质又可划分为单前陆、双前陆及走滑前陆等盆地;
            • The geodynamic environment in which foreland basin is developed is rather limited both temporally and spatially in the geological history.
              在地质历史上,适于前陆盆地发育的地球动力学环境,在时间和空间上均是相当有限的。
            • The Formation of the salt tectonics in the Kuqa foreland fold belt may be controlled by compression, gravitational gliding and gravitational spreading.
              库车前陆褶皱带盐构造的形成可能受挤压作用、重力滑动和重力扩展作用多重控制。