1) Jianghan Dongting basin
江汉洞庭盆地
1.
By using the results of tectonic analysis, focal mechanism solution and site geo stress survey we get the predominant distribution of principal stress of tectonic stress field in the Jianghan Dongting basin and its vicinal areas in four periods since Cenozoic.
利用构造分析结果、震源机制解和现场应力测量资料 ,获得江汉洞庭盆地及邻区新生代 4个时段构造应力场主应力的优势分布。
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) Jianghan Basin
江汉盆地
1.
Diagenesis of anhedritite in the Cretaceous reservoir and its influence on the hydrocarbon distribution in southeast Jianghan Basin;
江汉盆地白垩系储集层中硬石膏的成岩作用及其对油气分布的控制
2.
Exploration potential contrast of non-sandstone reservoirs within salt-layers between Shashi and Qianjiang Formations,Jianghan Basin;
江汉盆地潜江组与沙市组盐间非砂岩油气藏勘探潜力对比
3.
Characteristics of pore structures and oil production potential of sandstone reservoir of Paleogene Xingouzui Formation in Jianghan Basin;
江汉盆地新沟嘴组砂岩孔隙结构与产油潜力
5) the Jianghan Basin
江汉盆地
1.
Based on the distribution characteristics of proven oil field reserves size and the changing trend of oil yield and discovery rate per exploration well over the years in the Qianjiang Sag,the Jianghan Basin,three different kinds of statistic methods such as pool size sequence,Weng's life cycle and exploration benefit method have been chosen in the paper.
根据江汉盆地潜江凹陷已探明油田储量规模分布特点、历年石油产量和单井发现率数据变化趋势,选用了油田规模序列法、翁氏生命旋回法和勘探效益法3种统计方法,在分析不同方法的数学原理、数学模型、参数特征及适用条件的基础上,从不同侧面计算潜江凹陷石油资源量。
2.
Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.
组成江汉盆地潜江凹陷潜江组盐间段非砂岩储层的岩石主要为泥晶白云岩、钙芒硝岩、泥岩及其混积岩,孔渗性普遍较差。
3.
The bulk rock analysis technology of organic petrology was used in this paper to systematically study the maceral composition, hydrocarbon generating components and organic thermal evolution of the Lower Tertiary source rock in the Jianghan Basin.
作者采用有机岩石学全岩分析技术 ,系统研究了江汉盆地下第三系烃源岩的显微组分组成、生烃组分及有机质热演化。
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：洞庭送李十二赴零陵
【诗文】：
今日相逢落叶前，洞庭秋水远连天。
共说金华旧游处，回看北斗欲潸然。
【注释】：
【出处】：
全唐诗：卷235_34
今日相逢落叶前，洞庭秋水远连天。
共说金华旧游处，回看北斗欲潸然。
【注释】：
【出处】：
全唐诗：卷235_34
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条