1) paralagoon
边缘泻湖
2) lagoon reef margin
泻湖礁边缘
3) lake rim
湖盆边缘
4) lagoon
[英][lə'ɡu:n] [美][lə'gun]
泻湖
1.
Based on the stratigraphic, structural features and the types of ore deposits in Lingshi, it is concluded that the gypsum was deposited in supratidal lagoons.
根据灵石石膏矿区的地层、构造特征，矿床特征及矿石类型等对矿床的成因进行了分析探讨，认为该矿床是在潮上泻湖中沉积而形成。
2.
Sedimentological studies of coal-bearing member of Ceshui Fomation inLengshuijing coal mine indicate that it is sediments of depositional system of barrier is-land-lagoon and shows vertical sequence from regression to transgression,Coalaccumulation is influenced by depositional environments in a great degree.
本文依据对冷水江矿区测水组含煤段的沉积环境分析，提出该段为障壁岛──泻湖体系的沉积、垂向上表现为海退序列─—海进序列。
3.
The Zhanjiang Bay can be regarded as a tidal inlet system of drowned valley lagoon type.
湛江湾是一溺谷—泻湖型的潮汐通道系统，着重讨论了围海造地与该系统的关系，特别指出１９５８年的南三岛的联围，使湛江湾扩大了纳潮面积，完善了潮汐通道系统。
5) extensional lacustrine basin margin
伸展型湖盆边缘
1.
In the Bohai Sea area,the structural styles of the Paleogene lacustrine basin margin can be divided into two types:extensional lacustrine basin margin and strike slipping lacustrine basin margin and the former one is further subdivided into the steep slope faulted lacu.
渤海海域古近系湖盆边缘构造样式可划分为伸展型湖盆边缘和走滑型湖盆边缘两大类,伸展型湖盆边缘又可划分为陡坡断裂型湖盆边缘、缓坡断裂型湖盆边缘、简单缓坡带型湖盆边缘和轴向斜坡型湖盆边缘。
6) strike slipping lacustrine basin margin
走滑型湖盆边缘
1.
In the Bohai Sea area,the structural styles of the Paleogene lacustrine basin margin can be divided into two types:extensional lacustrine basin margin and strike slipping lacustrine basin margin and the former one is further subdivided into the steep slope faulted lacu.
渤海海域古近系湖盆边缘构造样式可划分为伸展型湖盆边缘和走滑型湖盆边缘两大类,伸展型湖盆边缘又可划分为陡坡断裂型湖盆边缘、缓坡断裂型湖盆边缘、简单缓坡带型湖盆边缘和轴向斜坡型湖盆边缘。
补充资料：湖盆
| 湖盆 lake basin 地表上汇集水体的相对封闭的洼地。形似盆状。湖盆成因有地壳运动形成的，如断陷湖盆、坳陷湖盆；还有外力作用形成的，如冰蚀湖盆、堆积湖盆等，此外也有人类经济活动形成的，如水库库区等。湖盆可以由5部分组成：湖岸、沿岸带、岸边浅滩、水下斜坡、湖盆底。湖泊面积的大小，湖盆地质条件和水流动态不同，湖盆的形态也有差异。研究湖盆的形态及其变化，有助于了解湖泊的起源、发展；湖泊的容积、湖水的理化性质和水文形势的变化。 |
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参考词条