The Tarim gas province consist of two major gas regions (Tabei kuqa and Taxinan).
塔里木气区包括塔北—库车气区和塔西南气区两大部份。
Kuqa basin have wide thick rock salt, potassium can be as into the material foundation;
库车盆地有广厚的石盐岩层，可以作为成钾的物质基础；
Kuqa depression in Tarim basin has the basic geologic conditions to form medium and large gas pools.
塔里木盆地库车坳陷具备大中型天然气藏形成的基本地质条件。
Kuqa County Hospital for Infectious Diseases will be responsible for Kuqa, Xayar, the new and, Baicheng AIDS treatment.
库车县传染病医院将负责库车、沙雅、新和、拜城艾滋病患者的治疗。
The discovery of Kala-2 gas field reveals a good exploration prospect of the Cretaceous formation in the Kuqa depression.
克拉2大气田的发现，展示了库车坳陷白垩系良好的油气勘探潜力。
The exploration revealed that the Kuqa foreland depression was becoming an important giant gas accumulating area by degrees.
随着勘探的深入，库车前陆坳陷逐渐成为我国重要的大气区。
The Jurassic coal in Kuqa Depression has high gas potential and mainly produces methane at the high thermal evolution stage.
库车坳陷侏罗系煤具有高的产气性，在高演化阶段主要产甲烷气；
The stratigraphic overlap traps in the south margin of the Kuqa Depression is a favourable target for hydrocarbon exploration.
因此库车坳陷南缘地层超覆圈闭具有良好的含油气前景。
The physical chemical conditions of oil gas migration in the Kuqa foreland basin were studied with fluid geology method in this paper.
本文运用流体地质学方法研究了库车前陆盆地油气运移的物理化学条件。
Fold-thrust belts and salt-related structures are very prevalent in the Kuqa foreland fold-thrust belt of Tarim Basin in Northwest China.
褶皱-冲断带和盐相关构造均十分发育的秋立塔克地区构造极其复杂，该地区新生界内部存在两套起滑脱层作用的膏盐层。
In the Kuqa fold-thrust zone, a lateral ramp-related displacement transfer structure is developed in the eastern Qiulitag structural belt.
库车褶皱冲断带东秋里塔格构造带发育与侧断坡有关的位移转换构造。
The Kelasu triangle zone occurs under the Paleogene evaporites in Kelasu anticline zone of Kuqa thrust-and-fold belts, Tarim basin (Northwest China).
塔里木盆地库车褶皱冲断带克拉苏构造带在古近系膏盐岩之下发育克拉苏三角带。
The applied case comparison of the old and new models in Kuqa Depression proves the rationality and practicability of the compaction-filtration model.
两种模型在库车坳陷进行了对比应用，证实了压实渗流模型的合理性和实用性。
The Formation of the salt tectonics in the Kuqa foreland fold belt may be controlled by compression, gravitational gliding and gravitational spreading.
库车前陆褶皱带盐构造的形成可能受挤压作用、重力滑动和重力扩展作用多重控制。
A variety of salt-related structures have developed in the Kuqa foreland fold-thrust belt, in which the most fascinating structure is the salt nappe complex.
盐岩层的存在使库车前陆褶皱-冲断带发育-系列盐相关构造，其中最引人注目的是盐推覆构造。
The field observation and seismic data interpretation reveal that the displacement transfer zone is developed in the Kelasu triangle zone, Kuqa thrust-and-fold belts.
根据对库车褶皱冲断带的地面地质调查和地震反射剖面的解释表明，库车褶皱冲断带克拉苏三角带发育垂直构造走向的位移转换构造。
Kuqa rejuvenated foreland basin is located along the northern margin of Tarim basin. The characteristics of sedimentation and structures are of typical foreland basin.
库车再生前陆盆地位于塔里木盆地的北缘，其沉积和构造特征具有典型的前陆盆地性质。
It is suggested that the tectonic compression is one of the main factors resulted in the incremental pore fluid pressure of Mesozoic reservoirs in northern Kuqa depression.
所有这些分析证实，构造挤压作用是导致库车坳陷北部中生界储集层流体增压的主要因素之一。
This uplifting not only resulted in the erosion or non-deposition of the Late Cretaceous strata, but also in the formation of the structural rudiment of deformation in the Kuqa Depression.
这一隆升过程不仅造成了库车坳陷全区缺失晚白垩世地层，而且也导致了库车坳陷构造变形雏形的发育。
This method is applied in the calculation of the stress in the Kuqa piedmont compressive area of the Tarim basin. The calculated result coincides with the result of the acoustic experiment.
应用该方法对塔里木盆地库车山前挤压应力区进行了实际计算，其结果与实验结果相符。
The subsurface structures of the Kuqa rejuvenated foreland basin are really complex, so a correct interpretation of them is the key for understanding the genesis of the basin and hydrocarbon traps.
库车再生前陆盆地地下构造复杂，正确的构造解释就成为了解盆地成因机理和油气圈闭的关键所在。
By comprehensive analysis on the characteristics of petroleum geology in the Kuqa Depression in this paper, it is pointed out that the Kuqa Depression has good pool forming conditions for natural gas.
本文通过对库车坳陷石油地质特征的综合分析，指出库车坳陷具有良好的天然气成藏条件。
The Late-Cretaceous uplifting process of the Kuqa Depression was investigated using the fission track (FT) technique and the geological analysis. The uplifting has occurred for about 89 million years.
利用裂变径迹分析技术，并结合地质学研究方法，对库车坳陷晚白垩世隆升过程进行了研究。
The Late-Cretaceous uplifting process of the Kuqa Depression was investigated using the fission track (FT) technique and the geological analysis. The uplifting has occurred for about 89 million years.
利用裂变径迹分析技术，并结合地质学研究方法，对库车坳陷晚白垩世隆升过程进行了研究。
应用推荐