塔里木盆地

Modified by the Tibetan and Pamir Plateau and the peripheral mountains, the inner China and the Tarim Basin experienced continuous aridification and desertification.

随高原和周边山地的隆升，中国内陆和塔里木盆地持续干旱化和沙漠化，沙漠逐步扩大至今天规模。

On the basis of analyzing the petrologic characteristics of Triassic reservoir in jilake area, Talim u basin, the pot tial factors of formation damage are discussed.

本文在分析塔里木盆地吉拉吉地区三叠系储层岩石学特征的基础上，探讨了潜在的地层损害因素。

The Well Yuli 1 is the first well which drills through Sinian System on the northeast margin of the Tarim Basin .

尉犁1井是塔里木盆地东北缘第一口钻揭震旦系的井，它的钻探分析对了解孔雀河古斜坡成藏条件、确定该区下一步有利勘探区具有重要的意义。

In this paper, the stress and strain fields of lithosphere in Himalayan Western Syntaxis orogenic belt and its adjacent areas since 10Ma are investigated through using the 3-D finite-element simulation, and deformation and evolution process in former 2Ma are simulated with different rheological parameters and rheological structure. Studies on functions in simulation process of different viscosity parameters, constitutive relation and changes of initial curst thickness show below results:(1) When various viscoelastic models are adopted, the selection of the coefficient of viscosity in the Western Syntaxis area has important influence on the its uplifts and evolutions. The computational results show that the viscosity in the Western Syntaxis area should be smaller than 1023Pa·s;(2) When the elastic model is adopted in relatively rigid Tarim basin, obvious changes are induced to the stress and strain fields of the whole Western Syntaxis area;(3) The existence of mechanical property stable block doesn′t make the propagation of the stress field show obvious decoupling phenomenon.

用数值模拟的方法探讨了自10 Ma以来喜马拉雅弧形造山带的西构造结及邻区岩石圈的形变和位移变化特征，并采用不同的流变参数和流变结构模拟了前2 Ma内的形变和应力场的演化过程，通过对不同黏性系数、本构关系和初始地壳厚度的改变在演化过程中所起的作用研究表明：（1）采用黏弹性模型时，西构造结区黏性参数的选取对西构造结及邻区隆升高度和隆升范围有重要影响，计算结果给出西构造结区地壳黏性系数应小于1023Pa·s；（2）相对刚性的塔里木盆地采用弹性结构时，对整个西构造结区域的应力和应变场均能引致明显变化；（3）力学性质稳定块体的存在并没有使应力场的传播出现明显的解耦现象。

Originating from Chang'an( the present-day Xi'an), the route traversed Shaanxi Province, the Hexi Corridor in Gansu Province, the Tarin Basin in Xinjiang, the Pamir mountain region, Afghanistan, Iran, Iraq and Syria, ending at the eastern shores of the Mediterranean.

这条通道源于长安城，一路穿越陕西省、甘肃省境内的河西走廊、新疆的塔里木盆地、帕米尔山区、阿富汗、伊朗、伊拉克以及叙利亚，最后抵达地中海的东岸，全程7千公里，其中有4千多公里的路段在中国境内。

The characteristics of the salt formation in Tarim Basin is deep, high temperature and high pressure, easy to result in the undergauge, collapse, drill bit or pipe sticking.

针对塔里木盆地石炭系盐层埋藏深，温度高，地层压力大，极易发生&缩径、坍塌&，造成卡钻，同时由于盐岩层的塑性蠕动，形成不规则井眼，甚至造成套管挤毁变形事故，井身质量难以控制，固井质量难以保证等问题，通过对同类型已钻井进行总结分析，提出了一系列钻井技术措施，并在T726井严格实施。

The physical chemistry properties of evaporite beds in Bachu area are analysed.On the basis of the feature of salt beds,the undersaturation salt water drilling fluid is determined.

塔里木盆地复合盐层地层分布广，在不同构造的钻探中都钻遇盐层，盐层厚度一般几十米到几百米，岩性以盐岩与膏岩、泥岩、泥质粉砂岩等不等厚互层。

Tarim basin suffered multi-stage tectonic transform and emplaced in the last tectonic movement.

塔里木盆地经历了多期构造变革，并在最后一次构造运动中定格。

This article analyses two kinds of oasis farming system of Talimu,connects the prestent developing situation of farm and discusses the development of faming system in the area in the 21 st century.

通过对塔里木盆地两类绿洲农作制度改革历史的分析，结合当前农业发展形势，对该地区 2 1世纪农作制度发展进行了讨论。

The tectonic units in the North part of Tarim are dextral permuted, which is mainly due to the trans compression force produced by the collision between Indian Plate and Eurasia Plate.

受印度板块和欧亚板块陆陆碰撞产生的区域规模剪切挤压应力影响，塔里木盆地北部各构造单元呈右旋斜列。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。