1) Relict sea basin
残余海盆
2) relict basin
残余盆地
1.
Types,features and studying method of continental relict basins;
陆相残余盆地的主要类型、特点及研究方法
2.
Based on previous researches, evolution mechanism and distribution characteristics of relict basins are stated.
在回顾残余盆地研究现状的基础上 ,从解剖残余盆地成因机制及其分布特征入手 ,详细阐述了残余盆地的研究思路及方法 ,提出研究残余盆地应以构造分析为主线进行 。
3.
The structural characteristics such as vertically stratigraphical sequence hiatus,planar sedimentary system and facies incompleteness,delimitation of a basin by erosion or fault,and the structural feature of outcrop in peripheral and near arears could be taken as marks in recognizing relict basins.
垂向上层序不完整 ,平面上沉积体系和相带不齐全 ,盆地以侵蚀或断层为边界以及周缘和邻近地区露头的构造特征都可作为识别残余盆地的标志。
3) remnant basin
残余盆地
1.
Mesozoic remnant basin characteristics and hydrocarbon exploration direction on East China Sea shelf;
东海陆架中生代残余盆地特征及勘探方向探讨
2.
Petroleum potential and exploration direction of pre-Tertiary remnant basins in Offshore China;
中国近海前第三纪残余盆地及其勘探潜力与方向
5) Residual real-arc basin
残余弧后盆
6) residual trough
残余海槽
1.
Based on the data of lithological association,petro-geochemistry and paleontology integrated with anal-ysis of geotectonic evolution and marine /continental change,this paper presents that the Late Permian Lucaogou forma-tion is lacustrine deposit modified by residual trough with aquifer medium of lake water formed by terrestrial facies.
从岩性组合、岩石地球化学、古生物等资料出发,结合大地构造演化和海陆变迁分析,提出三塘湖盆地上二叠统芦草沟组为残余海槽改造而成的湖相沉积,水体介质由海水逐渐淡化而成湖水,物源输入则以陆相为主。
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