1) marginal basins
边缘海盆
1.
There exist a series of marginal basins in the Western Pacific.
太平洋西缘分布着一系列边缘海盆。
2.
There exist in the western Pacific more than 75% marginal basins of the world.
从地球深部地幔流动引起的地质作用出发 ,结合裂谷的发展演化规律 ,认为地幔向东 (或南东 )的蠕散和流动促使亚洲大陆边缘地壳拉伸、变薄以致破裂 ,由大陆裂谷发展至弧后裂谷 ,形成西太平洋边缘海盆。
2) marginal basin
边缘海盆地
1.
During the Neoproterozoic to the Early Paleozoic, the South China was a marginal basin captured by the Yangtze active continental margin, filled with very thick flysch, sandstone, and shale sediments.
华南新元古代到早古生代是扬子活动大陆边缘构造“捕获”的一个边缘海盆地,其间充填了巨厚的复理石、砂、页岩沉积。
2.
The more than 75 percent of the marginal basins found in the Earth today are concentrated in the western pacific.
西太平洋集中发育了全球 75%的边缘海盆地 ,这些盆地形成于始新世、渐新世—中新世和晚中新世—第四纪 3个边缘海扩张幕。
3) Zhe-Wan Marginal Sea Basin
浙皖边缘海盆
4) evolution of back-arc basin
边缘海盆演化
5) East China Sea and South China Sea marginal basin
东海及南海边缘盆地
补充资料：海盆
深度在3,000—6,000米之间的海底盆地，除海岭和海沟外，底部平缓。海盆面积占海洋总面积的70%以上。
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