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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

            • 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。
            • Mesozoic-Cenozoic Superimposed Orogeny and Foreland Deformation in the Northeastern Sichuan Basin
              四川盆地东北部中&新生代造山与前陆变形构造叠合关系研究
            • A typical foreland basin was formed at the front of Kalatnayli mountain, northeastern margin of Junggar basin.
              准噶尔盆地东北缘于克拉麦里山前形成典型的前陆盆地。
            • Lower Paleozoic omission zone in Jiangnan uplift ── a sign of Caledonian Foreland Fold thrust belt
              江南隆起上的下古生界缺失带&华南加里东前陆褶冲带的标志
            • Laojunmiao structural belt is located in Cenozoic foreland thrust belt of south margin, Jiuquan basin, which is superposed over the south uplift and Shida depression of Early Cretaceous faulted basin.
              老君庙构造带是中国发现最早的老君庙油田所处的构造带,位于酒泉盆地南缘新生代前陆冲断带,叠置于早白垩世断陷盆地的南部隆起和石大凹陷之上。
            • The tectonic evolution and hydrocarbon accumulation in the foreland fold-and-thrust belt of the southern JunggarBasin is complex.
              准噶尔盆地南缘前陆冲断带构造演化与成藏过程复杂。
            • 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。
            • Western Sichuan Depression is a foreland basin developed in the west of Sichuan basin since late Triassic.
              川西坳陷是指四川盆地西部晚三叠世以来形成的前陆盆地。
            • 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。
            • The foreland basin of Late Paleozoic is accumulated by the Upper Devonian and Lower Carboniferous.
              晚古生代在前陆盆地率先接受了上泥盆统、下石炭统沉积;