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说明：双击或选中下面任意单词，将显示该词的音标、读音、翻译等；选中中文或多个词，将显示翻译。
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1) Sujiquan
苏吉泉
1.
Structural characteristics of triangle carbon mineral from Sujiquan graphite ore deposit,Xinjiang province,China;
新疆苏吉泉石墨中三角形碳矿物的结构特征
2) Yingjishu
英吉苏
1.
Yingjishu depression is located in the Easter of Tarim and exploration area amount to 15 X 104km2.
英吉苏凹陷位于塔里木盆地东部地区，勘探面积达15×10~4km~z。
3) Matsushima Sojnsen
松岛苏顺泉
4) Yingjisu sag
英吉苏凹陷
1.
Diagenetic evolution mode and formation mechanism of the gas reservoir in Yingjisu Sag;
英吉苏凹陷天然气藏成岩演化模式及成藏机理
2.
A two-stage mode of stable carbon isotopic profile of n-alkanes from crude oil in the Yingjisu sag of Tarim basin has been revealed, featuring a two-phase hydrocarbon accumulation process to date in this region.
塔里木盆地英吉苏凹陷目前所揭示原油分子碳同位素分布呈现明显二阶段模式,显示该地区具两期成藏特征:一期为以龙口1井为代表的正常原油成藏,油源主要与下奥陶统沉积有关(以英东2井4171-4175m地层为对比源岩);另一期为以英南2井为代表的高演化凝析油气成藏,其轻烃组成可能属于干酪根高演化阶段产物,而非原油裂解成因。
3.
Fluid history of Jurassic gas reservoir in Yingjisu sag is reconstructed and studied through testing hydrocarbon inclusions in reservoir rocks.
应用储层岩石烃类流体包裹体测试技术,对英吉苏凹陷侏罗系气藏进行了重建流体历史分析研究。
5) the Yingjisu Sag
英吉苏凹陷
1.
Through the studying of the structure background,source rocks,reservoirs and seals and preservation in the Yingjisu Sag in the east of Tarim Basin,the geologic conditions and main control factors of the accumulation are discussed.
通过对塔里木盆地东部英吉苏凹陷的构造背景、油源条件、储盖层条件、聚集和保存条件的分析,探讨了英吉苏凹陷天然气成藏的地质条件和成藏主控因素。
2.
The Yingjisu Sag, situated in northeastern Tarim Basin, was a part of the Central Asia-NW China superlarge Basin in Jurassic, and a cratonic basin (intracontinental depression) formed in Early Jurassic.
英吉苏凹陷位于塔里木盆地东北部,侏罗纪属中亚—中国西北超大型盆地的一部分,是早侏罗世形成的克拉通内盆地。
6) Yingjisu depression
英吉苏凹陷
1.
Yingjisu depression is a break-sinking basin that was developed on the low-Paleozoic denudation physiognomy.
英吉苏凹陷是一发育于早古生代剥蚀地貌背景上的中新生代断—坳型沉积盆地。
2.
Yingjisu depression lies in north of the Tarim basin as same as Kuche depression,they have the same deposit-tectonic evolution history.
英吉苏凹陷与库车坳陷同处于塔里木盆地北缘,三叠纪以来二者具有类似的沉积—构造演化历史。
3.
The Meso-Cenozoic Yingjisu depression is a piggyback foreland ba si n developed in the setting of the Paleozoic thrust nappe structure.
叠瓦式逆冲断层、花状构造、构造三角带、断展褶皱和披覆构造是英吉苏凹陷的主要变形样式。
补充资料：马斯吉德苏莱曼水电站
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