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1)  coastline recession causes
砂岸
2)  shore sand
岸砂
3)  bank sand
河砂,岸砂
4)  coastal mining sites
海岸砂矿
5)  sandy coast
砂质海岸
1.
From the 1960s to the 1990s, the erosional range of the east and west sandy coasts of Liaodong Bay was gradually expanded, and the coastal erosion was constantly aggravated, which made serious damage to the people s production and life.
通过现场调查和多年监测,分析了辽东湾东西两侧砂质海岸侵蚀的特点,认为海岸组成物质松散与海岸动力作用强烈是本区现代海岸侵蚀的基本条件,人为活动是关键因素,并提出了海岸侵蚀灾害的防治对策。
2.
Eastern China has a vast distribution of sandy coast that has multiple topographic forms and suffers from eolian hazards and coastal erosion and some other severe geologic problems, which has seriously blocked the development of social economy in the coastal areas.
中国东部砂质海岸分布范围广泛,地形发育多样,风沙灾害、海岸侵蚀等地质灾害问题多发,严重影响了沿海地区的社会经济发展。
3.
The paper reviews the progress in the researches on beach states, beach groundwater dynamics, sand bar dynamics, coastal dunes and nearshore processes in the sandy coast.
本文着重论述了在砂质海岸演变研究中,海滩状态,海滩地下水动力,砂坝动力学,海岸沙丘,近岸带过程等方面研究进展。
6)  shoreline sandbody
滨岸砂体
1.
shoreline sandbody,nearshore sandridge sandbody and offshore sandbody.
塔中志留系下沥青砂岩段沉积砂体的类型有滨岸砂体、近滨沙脊砂体和远滨砂体三种类型,正常条件下沉积的滨岸砂体具低角度交错层理和少量波痕,呈现出由粉砂岩—细砂岩—中细砂岩的反韵律变化特征。
补充资料:岸岸
1.每一处水岸。 2.严峻苛细。 3.高傲。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条