1、

Structural geologic characteristics of East China Sea Basin

东海盆地地质构造特征

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2、

Sediment Types and Sedimentation of the Central South China Sea Basin

南海中部沉积物类型和沉积作用特征

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3、

Geochemical differences between the oceanic crust of the South China Sea Basin and the ocean crust

南海中央海盆洋壳与大洋壳在地球化学上的差异性

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4、

The existence of marine Eocene strata from the East China Sea Basin and its significance

东海盆地海相始新世地层的存在及其意义

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5、

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。

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6、

The magnetic anomalies of the South China Sea Basin indicate that its oce.

南海盆地磁异常显示其洋壳是新老不一、厚薄不匀的新洋壳的拼合叠覆体。

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7、

After processing gravity and aeromagnetic data, we infer that the Haiyang Island and Liugong Island uplifts are connected by two smaller uplifts in NW direction, and these two smaller uplifts divide the North Yellow Sea basin into three parts.

通过重磁数据处理解释推测认为:两条NW向的次级隆起将海洋岛隆起与刘公岛隆起连接起来,同时将北黄海盆地分成3部分;

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8、

Some opinions on petroleum exploration in Cenozoic East China Sea Basin

关于东海新生代盆地油气勘探的若干见解

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10、

Application of hydrocarbon discharge quantitative analysis in target evaluation of South Yellow Sea Basin

油气充注定量分析技术在南黄海盆地目标评价中的应用

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11、

Genetic evolution and depositional filling model of tensional marginal sea basin: take the Pearl River Mouth Basin as an example

张性边缘海的成因演化特征及沉积充填模式&以珠江口盆地为例

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12、

During Middle Triassic, the Gejiu area was in a special sedimental environment, i.e. in a restricted marginal sea basin within the continental rift system.

中三叠世,个旧矿区处于特殊的沉积环境&陆裂谷系中的局限边缘海盆。

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13、

Metamorphic Rocks in the East China Sea Basin Bright Sun Yan

东海盆地的变质岩明亮孙岩

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14、

The formation of the marginal-sea basin would be related to the northward subduction of the lithospheric fault-block of South China with oceanic crustal sea areas at late pre-Cambrian and resulted from further extension of ancient marginal sea in the Sinian period.

这个边缘海盆地的产生与华南洋壳海域岩石圈断块在晚前寒武纪时期向北俯冲有关,是震旦纪古边缘海继续扩张的结果。

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15、

Formation and distribution of coal-rich unit of epicontinental sea basin in western Shandong

鲁西陆表海盆地富煤单元的形成与分布

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17、

The feature of the sedimentary succession of the epicontinental sea basin in the study area was analyzed by means of the stochastic math model, Markov chain.

运用马尔柯夫链随机性教学模型对研究区陆表海盆地沉积序列特性进行了分析研究。

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18、

Though Cenozoic link dextral pull apart rift system in the northwest Pacific margin basically inherited their original tectonic framework in post rifting period, they underwent some reformation, especially the Philippine Sea Basin.

西北太平洋边缘形成连锁右行拉分裂谷系统后,在后裂谷期它们虽然基本上继承了原来盆地格架,但遭到一定程度的改造。

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19、

Interannual Variations of the Upper Circulation in the Bering Sea Basin and Its Physical Mechanism

白令海海盆上层环流年际特征及初步机制研究

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20、

Of them, the D_2 deformation shows a consistent forming time, extensional direction and tectonic regime amongst the Dulong-Song Chay dome, South China block and the north margin of the South China Sea basin.

D2期构造在发育时间、伸展方向及变形方式等上既与华南地块同时期区域伸展构造特征相一致,也与南海盆地北缘早期扩张特征相一致。

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