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1)  East Sea God Religion
东海神
2)  Shendong
神东
1.
The Coal Resources and Using of Shendong Diggings;
神东矿区煤炭资源与利用
3)  East China Sea
东海
1.
Effects of Irradiance on Blooms of the Dinoflagellate Prorocentrum Donghaiense Lu in the Coastal Area in East China Sea;
光照在东海近海东海原甲藻赤潮发生中的作用
2.
Concept of Building the Ecological Environment Monitoring System of Coastal Wetlands in the East China Sea;
东海滨海湿地生态环境监测体系建设构想
3.
Exchange Rates of Dissolved Nutrients at the Sediment-Water Interface Before and After Diatom Bloom in the East China Sea in Spring;
东海春季赤潮前后沉积物-海水界面营养盐交换速率的研究
4)  the East China Sea
东海
1.
Basic characteristics and main controlling factors of P11 of F1 Block,Pinghu Field,the East China Sea;
东海放一断块P11层储层特征及其主控因素分析
2.
Seasonal Variation and Spatial Distribution of Nutrients and Their Relationships with Harmful Algal Blooms in Coastal Area of the East China Sea;
东海赤潮高发区营养盐时空分布特征及其与赤潮的关系
3.
Spatial and temporal distribution of the nutrients and its controlling factors in the high-frequency HAB occurrence area in the East China Sea;
东海赤潮高发区营养盐时空分布特征及其控制要素
5)  East Sea
东海
1.
Study on isolation of east sea marine bacteria which producing extracellular enzyme;
我国东海近海海域产胞外酶的海洋细菌的筛选
2.
China and Japan have had some difference about dividing the continental shelf of the East Sea and exclusive economic zone for a long time.
长期以来,中国与日本在东海大陆架与专属经济区的划分上存在着分歧。
3.
Characteristics of Moho is significant to deep structures in East Sea because Moho is important density inference between Crust and Mantle.
莫霍面是地壳和上地幔的分界面,是个重要的密度界面,东海莫霍面的展布特征, 对于研究东海深部构造具有重要意义。
6)  Donghai
东海
1.
Preliminary study on the genesis of rocked quartz in Donghai, Jiangsu province: evidences from fluid inclusions and Si, O isotope.;
江苏东海水晶矿床成因初探:流体包裹体和硅氧同位素证据
2.
The hydrocarbon migration and accumulation mode in the central anticlinal zone of Xihu depression, Donghai Basin is investigated by means of inclusion thermometry and authigenic illite dating data.
文章利用包裹体测温和成岩矿物伊利石测年数据资料,对东海盆地西湖凹陷中央背斜油气运移及成藏的基本模式进行了研究,认为中央背斜带储层流体包裹体明显分为盐水包裹体和有机包裹体,包裹体均一化温度分为3期,其对应的地质时间分别为中中新世、中新世晚期和上新世至第四纪。
3.
The anisotropy of thermal conductivity and its possible influencing factors are discussed for the rocks in Donghai area.
通过对面理发育的样品进行测试,东海地区各类岩石的热导率具有较明显的各向异性。
补充资料:东海神珠

在塔湾景区内龙珠滩海边,经过海浪长时期冲击,磨练成一颗直径80厘米的石球,称为“东海神珠”,龙珠在龙喉里吞吐翻滚,发出隆隆回声,编织出一幅美妙神奇的“金龙吐珠”图,被誉为“中华一绝”,这就是桃花岛12大景观之一的“金龙吐珠”。

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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