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1)  northern Jiangsu lowlands
苏北低地
1.
The system of northern Jiangsu lowlands has its particular states and structures due to the seariver interaction.
苏北低地位处我国沿海中部,地面平均高程3m左右,平均坡降多在0。
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)  North Jiangsu
苏北地区
1.
Distribution of Heavy Metals in the Soil-Rice System and Food Exposure Risk Assessment of North Jiangsu,China.;
苏北地区土壤-水稻系统重金属分布及其食物安全风险评价
2.
The Research and Practice of Energy SavingBuilding Technology in North Jiangsu;
建筑节能在苏北地区的研究与实践
3.
On North Jiangsu Gas Promotion Problems and Solutions;
浅谈苏北地区沼气推广的问题与对策
5)  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。
6)  northern Jiangsu province
苏北地区
1.
Analysis of Status of Tourism Talents Supply in Northern Jiangsu Province and Research of Its Countermeasures;
苏北地区旅游人才供给现状分析及对策研究
补充资料:北西伯利亚低地
北西伯利亚低地
North Siberian Lowland

   北亚低平原。位于俄罗斯境内奥列尼奥克河下游与叶尼塞湾之间。北起贝兰加山脉,南至中西伯利亚高原。西北临喀拉海,东北临拉普捷夫海, 沿海岸线曲折 ,多深裂海湾。东西长1400千米,南北宽600千米,海拔小于200米。河流纵横,湖泊众多,沼泽密布。较大河流有奥列尼奥克河、阿纳巴尔河、皮亚西纳河、上泰梅尔河、哈坦加河及其支流赫塔河和科图伊河等,均北流注入北冰洋。较大湖泊有皮亚西诺湖、拉巴兹湖、波尔特尼亚吉诺湖及泰梅尔湖等。其中最大湖泊泰梅尔湖,位于低地与泰梅尔半岛之间,面积4560平方千米,流经低地中部的上泰梅尔河注入湖中,故北西伯利亚低地又称作泰梅尔低地 。整个低地基本位于北纬 70°~75°之间,属极地长寒气候,冬季长7~8个月,1 月均温-35~-40℃,夏季最暖月在10℃以下。云量大,多阴天,蒸发弱,湿度大,多降雪,年均降水量100~250毫米。地面为永冻土,北部为苔原带,南部为森林苔原,并间有灌丛。
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