sea basin信息详情
海洋盆地
[海洋]海盆
basin───n.水池;流域;盆地;盆;n.(Basin)人名;(俄)巴辛;(法)巴赞
hand basin───洗手盆
emesis basin───[医]呕吐盆;盂盆
basin wrench───承盘扳钳
flysch basin───飞行基地
tyrol basin───蒂罗尔盆地
river basin───n.江河流域;[水文]流域
exhumed basin───剥露盆地
CHINA basin───中国盆地
South Yellow Sea basin can further be subdivided into northern depression, middle uplift zone and southern depression.───南黄海盆地进一步划分为北部坳陷、中部隆起区及南部坳陷。
Based on the structural geometry and kinematics of North Yellow Sea basin, the tectonic deformation style and geodynamic process of North Yellow Sea basin are studied.───以北黄海盆地构造几何学、运动学特征为基础,探讨了北黄海盆地的构造变形样式及动力学演化过程。
geography of the Ordovician period is that: the Hannan paleocontinent and the Bashan Mountain rise at the north, and the wide epicontinental sea basin lies in the south.───奥陶纪时期,本区处于北为汉南古陆与巴山隆起,南为广阔的陆表海盆地的古地理环境。
which might be caused by mantle uplift during NW-SE-trending sea floor spreading of the Southwest sea basin.───此界面可能是西南海盆北西—南东向海底扩张期间地幔上隆所引起的。
Carbonate cements are the most abundant authigenic minerals in the Palaeogene sandstones of Lishui sag, East China Sea basin.───碳酸盐胶结物是东海盆地丽水凹陷古近系储层砂岩中最为重要的自生矿物,主要类型为铁白云石和方解石。
Interpretation method of subsalt structures in significant thickness of salt beds, east merging of littoral Caspian Sea basin.───滨里海盆地东缘巨厚盐岩区盐下构造的解释方法研究
The faulting and the sedimentary history of the Baiyun Sag were also influenced by spreading in the South China Sea Basin.───白云凹陷的断裂活动和沉积演化史还受到南海海盆扩张活动的影响。
At the edge zone of platform and deep sea basin, there are reef flat reservoir and various diagenesis, it's good for reservoir develop.───在台地与深海盆的边缘带发育的礁、滩相为有利储层发育的相带。
In summary, Mesozoic seafacies sedimentary rocks in the Ancient South China Sea Basin have a very good exploration potential.───由此可见,南海盆地中生代海相沉积岩具有较好的勘探潜力。
The natural geography of the Ordovician period is that: the Hannan paleocontinent and the Bashan Mountain rise at the north, and the wide epicontinental sea basin lies in the south.
The regional variety of development degree and horizon shows that the turbid-water with mud is from Cathysia on the east of Zhejiang-Anhui Sea Basin.
The four-order sequence of epicontinental sea basin is composed of two units, that is, the Transgressive System Tract (TST) and Highstand System Tract (HST).
During Devonian Period, the old sea basin of Qinling range was a continental sea, which was situated between Northern China and Yangtz old land.
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