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1)  isaxonine
伊沙索宁
2)  Eliel Saarinen
伊利尔·沙里宁
3)  YI Sha
伊沙
1.
On the Poems of YI Sha;
诗歌也是挑战——伊沙诗歌简论
4)  Yining depression
伊宁凹陷
1.
Permian petroleum system and exploration targets in Yining depression, Xinjiang, China;
伊宁凹陷二叠系油气系统与勘探目标
2.
Tiemulike Formation in the Permian above Yining depression is mainly composed of hydrocarbon source rocks which has formed two complete oil-bearing systems of P 2t-P 2t self-generation & self-reserving and P 2t-T 2-3 lower intervals generation and upper interval reserving.
伊宁凹陷以上二叠统铁木里克组为主要烃源岩 ,形成了P2 t-P2 t自生自储和P2 t-T2 -3 下生上储两套含油气系统。
3.
The origin of forming multiple waves in Yining depression in Yili basin is analyzed in this paper.
本文对伊犁盆地伊宁凹陷产生多次波的成因进行了分析 ,结合该区 2 0 0 0年宽线采集的地震资料处理过程 ,对压制多次波的方法进行了有益的探讨 ,利用拉冬域滤波方法结合内切除 ,对衰减伊宁地区多次波有明显效果 ,为今后压制多次波提供了有效的处理方法和借鉴经
5)  Yining Basin
伊宁盆地
1.
Jurassic Coal-bearing Strata and Coal-forming Patterns in the Yining Basin;
伊宁盆地侏罗系含煤地层及聚煤规律
2.
Analysis of Red Beds in Yining Basin and Coal Looking Orientation
伊宁盆地的“红层”与找煤方向
3.
The simulation results of Jurassic coal-measures in Yining Basin, Xinjiang show that when simulation temperature is 380 - 420℃ , hyrocarbon generation reaches its peak stage, and hydrocarbon generation stops at the temperature 450 - 500℃ To compare with lipti.
新疆伊宁盆地侏罗系煤系的模拟结果表明,基质镜质体在模拟温度为380~420℃时为生烃高峰期,450~500℃时生烃结束。
6)  Yining city section
伊宁市段
1.
The change law, pollution characteristics and causes of formation are discussed on the basis of synthetic evaluation of water quality situation over the years in Yining city section.
在对伊犁河伊宁市段历年水质状况进行综合评价的基础上 ,探讨了城市河段水质的变化规律、污染特征和成因。
补充资料:伊沙
【伊沙】
 (地名)I^sa山名。译曰自在。见增一阿含二十三。【又】(天名)伊沙那之略。(参见:伊舍那)
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