1) Hanasi basin
哈纳斯盆地
1.
Geochemistry and zircon U-Pb age of volcanic rocks from the Hanasi basin in the northern Xinjiang and their tectonic significance;
新疆北部哈纳斯盆地火山岩地球化学特征、锆石U-Pb年龄及其构造意义
2) Tuha basin
吐哈盆地
1.
Flow Unit Classification of Mid-Jurassic Reservoir in Qiudong Condensate Gas Reservoir,Tuha Basin;
吐哈盆地丘东凝析气藏中侏罗统储层流动单元划分
2.
Development characteristics and geneses of the fractures in low-permeability sandstone reservoir in the nothern depression of Tuha Basin;
吐哈盆地北部凹陷低渗透砂岩储层裂缝发育特征及成因
3.
Logging Interpreting Method Used for Extra-low Permeability Reservoirs in Tuha Basin;
吐哈盆地特低孔低渗油气层测井解释方法研究
3) Tu-Ha basin
吐哈盆地
1.
Analysis of Middle-Jurassic seismic facies in Hongtai area of Tu-Ha basin;
吐哈盆地红台地区中侏罗统地震相分析
2.
Characteristics of element geochemistry of Shuixigou Group in north-eastern Tu-Ha Basin;
吐哈盆地西南缘水西沟群沉积地球化学特征
3.
Discussion on reservoir prediction and reservoir-accumulating feature in Putaogou area of Tu-Ha basin;
吐哈盆地葡萄沟地区储层预测及成藏特征探讨
4) Turpan basin
吐哈盆地
1.
Sedimentary environments and petroleum resource of Jurassic rock in the Turpan Basin;
吐哈盆地侏罗系沉积特点及油气资源
2.
Determination of Tectonic Evolution of the Turpan Basin from Sandstone Components;
从砂岩成分探讨吐哈盆地构造演化
3.
Turpan basin is one of the largest coal basins of China.
通过对吐哈盆地不同类型烃源岩有机质及原油中微量元素的研究，并在与世界及我国其它地区原油对比的基础上，探讨了煤成烃中微量元素的分布规律，运用微量元素进行了油源对比的尝试。
5) Hami basin
哈密盆地
1.
Through seismic stratigraphic analysis on the northern area of Hami Basin, it is thought that there developed a set of alluvial fan fan delta shal low loch deposit system from north to south in the lower part of Badaowan format ion in Jurassic.
通过对哈密盆地北部地区进行地震地层学分析研究 ,认为该区侏罗系八道湾组下部由北向南发育了一套冲积扇—扇三角洲—滨浅湖沉积体系 ,其中丘状与楔状地震反射异常体为较典型的冲积扇沉积 ,并与其东南部的地层尖灭线构成地层岩性与构造相结合的复合圈闭。
2.
Surrounded by the llarkol Mountains, Karlik Mountains and Qoltag Mountains, Hami Basin is a large intermontane basin in the eastern part of the Tianshan Mountains.
本文对哈密盆地的现代地貌进行了成因分类，并系统地讨论了地貌结构特征，同时结合灾害地貌过程和资源特点提出了合理利用资源的几点意
6) Turpan hami Basin
吐哈盆地
1.
The geochemical analysis of underground water and fluid inclusion and the research on conditions for hydrocarbon migration and accumulation in Lukeqin structure, Turpan Hami basin have shown that: (1)the plaeo fluid in Tuyuke experienced stronger evaporation and rock fluid interaction while the plaeo fluid in Yudong and Lukeqin mostly experienced rain precipitation.
通过对吐哈盆地鲁克沁构造带流体包裹体和地层水化学成分以及油气运移和聚集条件的研究 ,认为 :①鲁克沁构造带流体地球化学演化表现为 :从古至今封存条件变好 ,现今地层水经历了相对于古流体更为强烈的流体 岩石相互作用 ,地层水矿化度和各种主要化学组分的含量增大 ,封闭条件比古流体更好。
2.
The theory of hydrocarbon expulsion threshold (HET) and basin simulation are applied to study on the characteristics of hydrocarbon expulsion from muddy source rocks of Triassic in Xiaoquangou area of Turpan Hami basin.
应用排烃门限控油气理论并结合盆地模拟 ,对吐哈盆地小泉沟群泥质烃源岩排烃门限和排烃特征进行了研究。
补充资料：纳来哈
纳来哈
Nalayh
Nalaiha纳来哈(N alayll)蒙古首都乌兰巴托卫星城市，重要产煤中心，空军基地。位于图勒河南侧，鸟兰巴托东南35千米处，北纬470 45‘，东经107“13‘。人口1.38万。地处图勒河谷，周围群l_IJ环抱。平均气温:1月一29.2℃，7月18.3℃。极端最低气温一48.9℃，最高38.3℃。年平均降水量250毫米。1915年开始采煤，1962年设市。工业以采煤为主，还有玻璃厂和发电站等。有铁路、公路通乌兰巴托，公路还通温都尔汗、乔巴山等地。空军基地位于市东南7千米处，标高1 300余米。跑道长约3000米，机场建有供航空兵部队飞行、生活及后勤补给等设施。(冯岳彬)
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