Xihu depression is situated at the middle of the Donghai shelf basin.
西湖凹陷位于东海陆架盆地中部。
The East China Sea Shelf Basin is a marginal sea basin located on Continental crust of China eastern margin.
东海陆架盆地是位于中国大陆东部边缘大陆地壳之上的边缘海盆地。
During late late Cretaceous-Eocene, volcanic island arc moved eastward and the east China Sea shelf basin was turned into a back-arc basin.
晚白垩世晚期—始新世,火山岛弧向东移动,东海陆架盆地变为弧后盆地。
In East China Sea shelf basin, the Mesozoic relict sediments are distributed in some central-south areas, such as Fuzhou sag, Minjiang sag and Yushan lower uplift.
东海陆架盆地中生界主要分布于盆地中南部的福州凹陷、闽江凹陷和渔山低隆起地区。
Limestone deposited in the whole inner shelf basin, including the swell belt, excepting a small mass of dolostone or dolomitic limestone could deposit in the center of basin.
包括隆起带上,仅(内)陆架盆地风暴浪基面之下中心位置有少量灰质白云岩和白云岩沉积。
The yields of acid hydrocarbon belong to medium to low abundance compared with those of the subaerial basins and the East China Sea shelf basin, and show weak geochemical field features.
酸解烃指标与整个中国陆上盆地和东海陆架盆地相比,属中等偏低丰度,呈现弱地球化学场特征。
The sedimentary facies type of Devonian in Baoshan-Shidian district consists of carbonate platform, shelf, slope and basin facies.
滇西保山—施甸地区泥盆系沉积相类型包括碳酸盐台地相、陆棚相反盆地相。
According to all of the results, we can concluded that, 1 the seismic sequences developed in the west shelf, trough basin and Ryukyu Island arc are different.
通过分析可以得出如下初步结论:1海槽南部西侧陆架、盆地内部以及琉球岛弧岛坡地震层序是不同的。
Wan 'an basin is a large scale Cenozoic sedimentary basin which is located on southwest shelf of the south China Sea.
万安盆地是南海西南部陆架上的大型新生代沉积盆地。
The geochemical characteristics of the metabasalt agree with those of continental rift type volcanic rocks, forming a tectonic environment of the active shelf rift basin.
变质玄武岩的地球化学特征与大陆裂谷型火山岩一致,形成于活动陆棚裂陷(谷)盆地的构造环境。
In the Jurassic and Cretaceous, generally it was also the shelf sea (shallow sea), but there were lacustrine and lagoonal environments in different parts of the basin.
侏罗纪-白垩纪在总的浅海陆棚环境下,盆地不同地区也形成了湖泊和潟湖环境。
Because of the difference of platform structure, platform, slope - shelf and basin have distinct diversities in facies constitution and longitudinal assembled sequence.
在不同台地结构型式下,台地相区、斜坡—陆棚相区以及盆地相区都有着不同的沉积响应,从而构成不同的沉积相纵向组合序列。
The Mesozoic in the East China Sea Shelf and Taixinan Basin has become a new area of petroleum exploration.
东海陆架和台西南盆地中生界业已成为油气勘探的新领域。
On the northern shelf of South China Sea, the latter assemblage can only be compared with the third member of Liushagang Formation in the WS1-3-1 well, Beibu Gulf Basin.
在南海北部陆架,这一孢粉组合可与WS1-3-1井流沙港组三段孢粉组合对比,时代为早始新世。
The Maantang Formation in western Sichuan basin was probably located in the shelf of the passive continental margin in Upper Triassic.
四川盆地西部在晚三叠世早期(卡尼期)为被动大陆边缘环境, 沉积岩石单元为马鞍塘组。
Two types of tempestites developed in beach and inner shelf environments respectively are discovered in Silurian system of Tazhong area, Tarim basin.
在大量岩心观察及岩相与环境分析的基础上,首次在塔中地区志留系识别出两种风暴沉积序列,它们分别产出于海滩和陆棚环境。
Two types of tempestites developed in beach and inner shelf environments respectively are discovered in Silurian system of Tazhong area, Tarim basin.
在大量岩心观察及岩相与环境分析的基础上,首次在塔中地区志留系识别出两种风暴沉积序列,它们分别产出于海滩和陆棚环境。
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