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1)  mid Kuqa
库车坳陷中部
1.
Application of broadened line plus large geophone array seismic technology in exploration in mid Kuqa;
宽线加大组合地震技术在库车坳陷中部勘探中的应用
2)  east part of the Kuqa depression
库车坳陷东部
1.
Based on analyses of outcrops, well logs and high-resolution seismic reflection data, the sedimentary systems types and distribution characteristics of the Cretaceous in the east part of the Kuqa depression were studied systematically.
通过对库车坳陷东部野外露头、钻井资料以及地震剖面的综合分析,对坳陷东部白垩系的沉积体系类型及其分布特征进行了系统的研究。
3)  Kuqa Depression
库车坳陷西部
1.
Control of Salt-Related Tectonics on Oil and Gas Accumulation in the Western Kuqa Depression;
库车坳陷西部构造圈闭形成期与烃源岩生烃期匹配关系探讨
4)  Kuqa depression
库车坳陷
1.
Abnormal pressure origin analysis of Kela 2 gas pool in Kuqa depression of Tarim basin;
库车坳陷克拉2气藏异常压力成因分析
2.
Geochemical Characteristics of Crude Oil from Frontal Uplift in Kuqa Depression;
库车坳陷前缘隆起带上原油地球化学特征
3.
Quantitative evaluation on contribution of structural compression to overpressure and analysis on origin of overpressure in Kuqa Depression;
库车坳陷构造挤压增压的定量评价及超压成因分析
5)  Kuche depression
库车坳陷
1.
Gas Reservoir Forming Patterns Conducted by Fractures in Kuche Depression;
库车坳陷断裂输导天然气成藏模式及作用分析
2.
Quantitative evaluation of the gas reservoir formation system of Jurassic-Tertiary in Kuche Depression;
库车坳陷侏罗系—第三系天然气成藏系统定量评价
3.
Inhomogeneity of oil and gas distribution and its controlling factors in Kuche Depression, Tarim Basin;
库车坳陷油气相态分布的不均一性及其控制因素
6)  The Kuqa depression
库车坳陷
1.
The Kelasu tectonic zone located in the Kuqa Depression of the Tarim Basin is rich in natural gas.
克拉苏构造带是库车坳陷天然气最富集的区带之一。
2.
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。
3.
Thermal simulation experiments of hydrocarbon generation on coal,mudstone and carbargilite samples of Triassic and Jurassic from the Kuqa Depression in the Tarim Basin were carried out through the temperature from 260 to 540 ℃ with 40 ℃ as increment.
选用塔里木盆地库车坳陷三叠系和侏罗系的煤、黑色泥岩及碳质泥岩等样品进行了260~540℃之间的生烃热模拟实验,模拟温阶为40℃,并对产物中天然气的碳同位素和实验后的固态产物的镜质体反射率进行了测定,得到了模拟气态烃产物中甲烷的碳同位素与模拟产物成熟度Ro的关系。
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