1) Shuangcheng Depression
双城凹陷
1.
Characteristics of Faults and Their Control to Hydrocarbon Migration in Shuangcheng Depression;
双城凹陷断裂特征及其对油气运聚的控制
2) Yancheng depression
盐城凹陷
1.
Study on accumulation stage of Zhujiadun Gas Pool in Yancheng Depression in Subei Basin;
苏北盆地盐城凹陷朱家墩气藏成藏期次研究
2.
The Characteristics of Natural Gas Accumulation in Zhujiadun Area of Yancheng Depression;
盐城凹陷朱家墩天然气成藏特征
3.
Key Gas-bearing Reservoirs in Yancheng Depression;
盐城凹陷主要含气储层研究
3) Yancheng Sag
盐城凹陷
1.
The origin of natural gas in Yancheng sag.;
盐城凹陷天然气藏成因研究
2.
Genetic Type of the Natural Gas From Yancheng Sag in North Jiangsu;
苏北盐城凹陷天然气成因类型
3.
An application of the K-V fingerprint technique to geochemical hydrocarbon prospecting in Yancheng sag, North Jiangsu basin;
K-V指纹技术在苏北盐城凹陷油气化探中的应用
4) the Yancheng Sag
盐城凹陷
1.
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。
5) Zhucheng sag
诸城凹陷
1.
Three layers are present in the middle and upper crusts in the northern border of Sulu orogenic belt, as revealed by the S-N-strike reflecting seismic profiles that cross the Zhucheng sag.
横穿诸城凹陷的南北向反射地震剖面揭示,苏鲁造山带北侧边界的中上地壳中存在着三层结构,即上部的胶莱盆地沉积盖层、中部的苏鲁楔状地体和下部代表华北板块的胶北地体;诸城凹陷边缘和内部断裂均显示同沉积正断层性质,苏鲁楔状地体中发育一组向北仰起的叠瓦状逆冲断层,而胶北地体显示了向南俯冲的态势。
6) Baicheng sag
拜城凹陷
1.
Firstly, based on the basin prototype, the Triassic and Jurassic mudstone and coal, the main source rocks of the basin, did not develop better in Baicheng sag than in the northern thrust belt including Keyi structural belt; Secondly, because of the thrusting happened in late Cenozoic, the Triassic and Jurassic source rocks reach to a high to .
从盆地构造史研究的角度认为库车盆地的天然气主要来源于北部山前冲断带:(1)受原型盆地构造格局的制约,三叠系、侏罗系烃源岩发育的最有利位置不是在拜城凹陷,而是在克依构造带及其以北的北部山前冲断带;(2)晚第三纪以来的逆冲推覆作用使得烃源岩提早进入高—过成熟阶段,并以产气和凝析油为主;(3)逆冲推覆作用所产生的北倾逆断层控制天然气自下而上、自北而南运移,位于运移路线上的克依构造带和秋里塔格构造带的东段与烃源岩的排气期匹配较好,从而使这些地区最富集天然气。
补充资料：2,2-双氯甲基-三亚甲基-双[双(2-氯乙基)磷酸脂]
CAS：38051-10-4
分子式：C13H24Cl6O8P2
中文名称：2,2-双氯甲基-三亚甲基-双[双(2-氯乙基)磷酸脂]
英文名称：2,2- bis(chloromethyl)-trimethylene bis[bis(2-chloroethyl)phosphate]
phosphoric acid, 2,2-bis(chloromethyl)-1,3-propanediyl tetrakis(2-chloroethyl)
2,2-bis(chloromethyl)trimethylene bis(bis(2-chloroethyl)phosphate)
2,2-bis(chloromethyl)-1,3-propanediyltetrakis(2-chloroethyl)phosphate
分子式：C13H24Cl6O8P2
中文名称：2,2-双氯甲基-三亚甲基-双[双(2-氯乙基)磷酸脂]
英文名称：2,2- bis(chloromethyl)-trimethylene bis[bis(2-chloroethyl)phosphate]
phosphoric acid, 2,2-bis(chloromethyl)-1,3-propanediyl tetrakis(2-chloroethyl)
2,2-bis(chloromethyl)trimethylene bis(bis(2-chloroethyl)phosphate)
2,2-bis(chloromethyl)-1,3-propanediyltetrakis(2-chloroethyl)phosphate
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