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1)  Suhongtu basin
苏红图盆地
1.
Mechanism research on uranium mineralization in basalt rock in Suhongtu basin;
苏红图盆地玄武岩中铀矿化机制研究
2)  Subei Basin
苏北盆地
1.
Characteristics and Interpretation of Gas Logging Data in Subei Basin;
苏北盆地气测资料特征及其解释应用
2.
Quantitative evaluation of the sealing capacity and identification of the preferred petroleum migration path in the Qintong subbasin, Subei basin;
苏北盆地溱潼凹陷断阶带油气运移路径综合分析
3.
An evaluation of the source bed in Upper Cretaceous Taizhou Formation,Subei basin;
苏北盆地上白垩统泰州组烃源层评价
3)  the Northern Jiangsu Basin
苏北盆地
1.
Based on studies of regional seismic profiles and conglomerate distribution characteristics,original deposition boundaries of the Northern Jiangsu Basin during late Cretaceous are confirmed.
通过研究区域地震剖面、砂砾岩分布特征等,确定苏北盆地晚白垩世原始盆地沉积边界;研究重矿物分布特征、砂岩体展布特征及联井剖面等,确定当时的沉积物源方向;通过区域地震相与单井相的结合,来恢复全区沉积相,进而恢复当时的原型盆地。
2.
In order to learn the dominating factors of surface expressions from hydrocarbon microseepage,surface geochemical explorations with free gas and headspace gas methods have been made over the Zhujiadun Gas Field,the Yancheng Sag,the northern Jiangsu Basin.
为了研究油气藏中烃类垂向微渗漏近地表异常显示的主要受控因素,在苏北盆地盐城凹陷朱家墩气田上方近地表开展了以游离烃、顶空气法为主的地球化学勘探研究。
3.
The Taizhou Formation reservoir in the Caoshe Oil Field of the Qintong Sag of the Northern Jiangsu Basin is a complex fault block reservoir.
苏北盆地溱潼凹陷草舍油田泰州组油藏是一个复杂断块油藏,边界断层遮挡性较好,内部小断层则基本不封闭,储层连通性较好。
4)  the North Jiangsu Basin
苏北盆地
1.
There are three types of shallow reservoirs controlled by different key factors for hydrocarbon accumulation in the North Jiangsu Basin,respectively controlled by low maturity and high efficiency oil source rock in the lower-middle part of the Fu2 Member,fault of vertical migration pathway,and large scale sandstone for lateral migration.
苏北盆地发育3种具有不同成藏主控因素的浅层油气藏,分别是阜二段中下部低熟高效烃源岩型、断裂垂向通道型及大型砂体侧向运移型浅层油气藏。
2.
Researches on burial,temperature,maturity and oil generation histories of hydrocarbon source rocks of Taizhou Formation in the Gaoyou Sag,the North Jiangsu Basin with basin modeling methods have indicated that,hydrocarbon source rocks of Tai2 Member have entered mature stage and Ro has reached 0.
运用盆地模拟方法,对苏北盆地高邮凹陷泰州组烃源岩的埋藏史、温度史、成熟度史及生油史进行研究发现,三垛早期,泰二段烃源岩进入成熟阶段,Ro达0。
3.
There are many micro-fractures in the CA Oilfield in Gaoyou Sag,the North Jiangsu Basin.
苏北盆地高邮凹陷CA油田微裂缝比较发育,但由于微裂缝发育规模、开度和延伸长度均较小而不易识别,研究方法和手段受到很大限制,研究起来难度较大。
5)  Northern Jiangsu Basin
苏北盆地
1.
Grain Size Characteristics and Their Paleo Environmental Significance of Xinghua 1# Core Sediments in Northern Jiangsu Basin, China;
苏北盆地兴化1#钻孔的沉积物粒度特征及其古环境意义
2.
Study on the Changes of Palaeoenvironment and Palaeoclimate during the Past 3Ma Recorded in Xinghua Core at Northern Jiangsu Basin;
苏北盆地兴化钻孔近3Ma环境变化记录研究
3.
Element Records of Environment Change in the Past 780ka from the No.1 Borehole Sediments of Xinghua, Northern Jiangsu Basin, China;
苏北盆地兴化1孔元素反映的中更新世以来的环境变化
6)  Zhaosu Basin
昭苏盆地
1.
Analysis on ore-formation conditions of sandstone-type uranium deposits in Zhaosu Basin——Comparison between Zhaosu Basin and Yili Basin;
昭苏盆地砂岩型铀矿成矿条件分析——昭苏盆地与伊犁盆地对比
2.
According to data of geochemical prospecting, the author contend that the geochemical environment of Zhaosu basin's soil lies still in primary level through compare, analysis and research of geochemical feature of general environment and primary environment and secondary environment of Zhaosu basin's soil.
利用区域地球化学勘查资料,通过对比、分析、研究昭苏盆地的土壤总体环境、原生环境和次生环境的地球化学特征,认为昭苏盆地土壤地球化学环境仍处于初始状态,大多数元素在风化、搬运、沉积、成土过程中无明显富集或贫化,人类的生产生活活动未显著改变原生土壤环境。
3.
By comprehensive analysis of CSAMT data in the Zhaosu Basin, some new ideas about the basement relief and geological structure of the Zhaosu Basin have been put forward in the paper.
通过对昭苏盆地CSAMT测量资料进行综合分析,对昭苏盆地的基底起伏、地质构造特征提出了一些新的看法。
补充资料:红脚鲣鸟(图)

    别名 鲣鸟

    学名 Sula sula

    英文名 Red-footed booby

    鲣鸟科 Sulidae

    分布 西沙群岛

    国家二级保护动物

    游禽。全长75厘米左右。通体大都呈白色。雄鸟两翅黑褐色。雌鸟背、腰和尾上覆羽染灰褐色,尾羽先端白。面盘侧裸皮黄色。嘴灰蓝,基部转为粉红或仅稍缀以红色。爪红色。

    营海洋群集生活。翅尖长,善飞行。繁殖期从3月至初秋。营巢于石滩或岛屿上的矮灌木和乔木上,偶亦在地面筑巢。每窝产卵1-2枚,椭圆形,表面粗糙,色青白。育雏期间,新鸟反刍胃内食物哺喂雏鸟。

 

 
 

 
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