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1)  Dongting diwa
洞庭地洼
2)  western margin of the Dongting diwa
洞庭地洼西缘
1.
There is a close relationship between occurrence of nonmetallic minerals and tectonic evolution of geosyncline,platform and diwa(geodepression)on the western margin of the Dongting diwa.
洞庭地洼西缘非金属矿产的产出特征与地槽、地台及地洼构造的演化具有密切的关系。
3)  Dongting basin
洞庭盆地
1.
Research on the Quaternary Laterite and Paleoclimate in the Dongting Basin;
洞庭盆地第四纪红土地层及古气候研究
2.
Genesis of Reticulate Clay in the Laterite of the Dongting Basin;
洞庭盆地红土地层中网纹的成因探讨
3.
Dongting basin in the middle of Jiangnan uplift belt of Yangzi paraplatfoim is a rift-subsidence to downwarped continental depositional basin, where two sets of source rock, ie Permian and lower Teriary, have developed.
洞庭盆地位于扬子准地台江南隆起带的中段,是白垩纪-第三纪时期,西太平洋板块向亚洲大陆俯冲,造成壳幔再度调整,深部地幔挤压和浅层地壳拉张,在两种应力场背景之上发生、发展起来的断陷—坳陷型內陆沉积盆地。
4)  Dongting Lake wetland
洞庭湖湿地
1.
Research on pattern for biology utilization and agriculture development in Dongting Lake wetland;
洞庭湖湿地生物利用与农业开发模式研究
2.
Community structure and diversity of birds on east Dongting Lake wetland of Hunan Province;
东洞庭湖湿地鸟类群落结构及其多样性
3.
In this paper the main ecological and environmental problems and their causing mechanisms in the Dongting Lake wetland are analyzed according to new investigations and observations.
依据 1999─ 2 0 0 1年的监测和调查资料 ,分析了洞庭湖湿地的生态环境问题及其形成机制 。
5)  Dongting lake area
洞庭湖地区
1.
The prevalent factors of schistosomiasis in the Dongting Lake area is very complex, and the complexities is because of the inextricably link between regional production、residents living and regional environment among the Lakes areas.
洞庭湖地区血吸虫病流行因素很复杂,复杂性在于湖区居民生产、生活与湖区环境产生的千丝万缕的联系,如果没有政府的主导性作用,切断血吸虫病的传播途径,控制疫情的蔓延是不可想象的难题。
6)  Dongtinghu Basin
洞庭湖盆地
1.
Using the data obtained from seismic, well log, and assaying, the research is conducted on sequence stratification and sedimentary facies of Taoyuan Formation, Yuanjiang Formation, Hanshou Formation, and Xinhekou Formation of Paleogene inYuanjiang sag in the Dongtinghu Basin.
通过地震、测井和分析化验等资料,对洞庭湖盆地沅江凹陷古近系古新统桃源组及始新统沅江组、汉寿组及新河口组进行层序地层和沉积相研究,首先可将古近纪划分为2个Ⅲ级层序、5个体系域,桃源组和沅江组构成层序I,汉寿组和新河口组构成层序Ⅱ。
补充资料:东洞庭山
      太湖中的半岛,太湖十三景区之一。位于江苏省吴县西境,亦称洞庭东山,简称东山。原为太湖中岛屿,西与西洞庭山对峙,与东岸陆地一衣带水。清雍正年间在人工围垦下渐淤而与陆地相连成半岛。以渡村为界,面积约60平方公里。相传隋将莫釐屯此,又名莫釐山。另据《越绝书》,伍了胥尝迎母居此,古称胥母山。山体为泥盆系砂岩构成的单面山,东南陡峭、西北平缓,主峰莫釐峰(一名大尖顶)海拔293米。 与西洞庭山和马迹山同为太湖名胜和亚热带经济林木栽培基地,产柑橘、枇杷、杨梅等果品和名茶"碧螺春"。有环山公路通半岛各村镇。名胜古迹有紫金庵、轩辕宫和陆巷明建筑群等。东山镇为经济中心,有公路经木渎镇达苏州市。
  

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