Analysis of Hydrocarbon Prospecting Domain in Tabei Uplift of Tarim Basin

The characteristics and kinetic modeling of carbon isotope of methane in Jurassic humic gas in Kuqa depression in Tarim basin have been studied by combining pyrolysis experiment in closed gold tube system and analysis of methane isotope with GC-IRMS isotope mass spectrograph.

应用黄金管封闭体系热解实验，结合GC IRMS同位素质谱仪的甲烷碳同位素分析，研究了塔里木盆地库车坳陷侏罗系煤生成甲烷的碳同位素特征及其动力学模拟。

Early Carboniferous foraminifera from northern margin of Tarim Basin, Xinjiang

塔里木盆地北缘早石炭世有孔虫

The impact of global change on net primary productivity ( NPP) and community succession of salinized meadow in north of Tarim Basin was discussed.

本文探讨了全球变化对塔里木盆地北部盐化草甸净第一性生产力（N PP）和群落演替的影响。

The latest result of oil and gas resource assessment is that the total resource is 123.37 million tons equivalent, which oil is 59.94 million tons and gas is ( 79 599.43) million cubes.

最新评价结果是塔里木盆地油气总资源量为123.37亿t油当量，其中油资源量为59.94亿t，天然气资源量为79599.43亿m3。

The V shape coupling relationship between the basin and the range is located between the Tarim basin and the West Kunlun tectonic belt, just above the upwarped area of Moho.

塔里木盆地南缘与西昆仑构造带间呈V型盆山耦合关系，其下方恰好是莫霍面上隆区。

The Moho discontinuity on the Tarim side is distinctly imaged sub-horizontally at depths of~ 44 km.

塔里木盆地的Moho界面非常清楚，近水平地位于~44km深度上。

It is shown that the Tarim basin ends at E91 ° longitude and no longer extends toward east.

指出塔里木盆地在E91°附近结束，不再向东延伸。

Miocene foraminifera of Tarim basin, Xinjiang and their geological significance

新疆塔里木盆地中新世有孔虫及其地质意义

The final model indicates that the thickness of the main part of Tarim basin varies in the range of 38~ 46 km. The model also reveals that the Moho dips southward beneath southern Tarim basin at an angle in concordance with the angle of the crystalline basement.

最终的模型显示塔里木盆地主体的地壳厚度为38～46km，而且塔里木南缘的Moho界面南倾，与结晶基底南倾的角度大体一致。

The temperature and pressure ranges for the gas condensate accumulations in the basin are 70-130 ℃ and 35-60? MPa, respectively.

塔里木盆地凝析气藏富集温度为70～130℃，压力范围为35～60MPa。

Diabase dikes exposed on the northwestern margin of the Tarim basin contain 44.34%-49.3% SiO2 have higher values of Na2O+ K2O ( 4.32%-6.04%) and Na2O/ K2O ( 2.23-9.15), showing the features of intraplate basalt.

塔里木盆地西北缘出露的辉绿岩墙的SiO2含量为44.34%～49.34%，Na2O+K2O（4.32%～6.04%）和Na2O/K2O均较高（2.23～9.15），主量元素反映板内玄武岩的特点。

Tectonic evolution in Northeast Tarim Basin and its relation to hydrocarbon

塔里木盆地东北地区构造演化及其与油气的关系

In MX area, Tarim basin, there are serious static mis ties between the seismic data collected in the early period of exploration and that in recent years because of the complex near surface conditions of desert.

塔里木盆地MX地区，地表为沙漠，复杂的近地表条件造成有些早期采集的老测线和新测线之间存在着严重的静校正闭合差。

Some Opinions about DST Flow Regime for Low Permeable Sand Stone Formation in Tarim Basin

对塔里木盆地低渗砂岩层DST测试工作制度的一点想法

The method by using SONN to auto-identify the seismic lithofacies from seismic data has been successfully applied in LGX oilfield of Tarim basin.

通过地震数据自动识别地震岩相，在塔里木盆地LGX油田应用取得了明显效果。

Geochronology of petroleum accumulation of Hade 4 oilfield, Tarim Basin

塔里木盆地哈得4油田成藏年代学研究

Depositional Palaeogeography of Cretaceous of Kuqa Depression in Northern Tarim Basin

塔里木盆地北部库车坳陷白垩系沉积古地理

Use of Rayleigh waves to study the layered crustal structure and q_r values of Tarim Basin in Xinjiang Province

用瑞利波研究新疆塔里木盆地地壳分层结构及Q R值

By using conventional meteorological data and the infrared and visible images of GMS-5 satellite, the floating dust weather from April 25 to May 4 in 1999 in Tarim Basin is analyzed.

根据常规气象观测资料、GMS5静止气象卫星的红外云图和可见光图像，分析了1999年4月25至5月4日塔里木盆地浮尘天气。

The main tectonic deformation in the Pamir Western Kunlun foreland fold and thrust belt started in Early Pliocene ( about 4.6 Ma ago), and migrated gradually from the orogen to the foreland basin, with the faulting and folding becoming younger and weakened in the basin.

帕米尔&西昆仑北麓前陆褶皱冲断带的主要构造变形时间始于上新世早期（距今约4.6Ma），断层、褶皱的变形时代由山前向盆地逐步变新，变形强度由山脉向塔里木盆地逐步减弱。