1·Ancient land reason massif crick of iron lie in southwest predestination of tarim basin.
铁克里克古陆缘地块位于塔里木盆地之西南缘。
2·Based on the authigenic and clay mineral assemblage, two types of diagenetic ambient have been recognized in the meso - cainozoic detrital rocks in tarim basin.
根据自生矿物与粘土矿物组合，在塔里木中新生界碎屑岩中可以识别出两种成岩环境。
3·A definite low Pn velocity region to the south of Tarim basin is possibly related to strong magma and tectonic activity.
塔里木南缘中部存在一显著的低速区，可能与岩浆活动和构造活动较强有关。
4·Tarim Basin is surrounded by mountains, the huge glaciers and snow hills on the high mountains are natural reservoir, which breed the forest grassland and many kinds of animals and plants.
塔里木盆地周围群山环抱，高山上巨大的冰川雪岭是天然水库，养育了森林草原和种类繁多的动植物。
5·This discovery will be greatly helpful in the researches on the basement tectonic of Tarim basin.
这一发现将对塔里木盆地基底构造的研究起到积极的推动作用。
1·Based on the data of tarim river basin this paper combines experiential and academic methods to calculate the irrigation quota of representative crops and develops relevant calculation system.
摘要利用塔里木河流域相关数据，采用经验与理论相结合的方法计算研究区代表作物的灌溉定额，并开发相应的计算系统。
2·Based on the data of Tarim River basin, this paper combines experiential and academic methods to calculate the irrigation quota of representative crops, and develops relevant calculation system.
利用塔里木河流域相关数据，采用经验与理论相结合的方法计算研究区代表作物的灌溉定额，并开发相应的计算系统。
3·The longest inland river in China — Tarim river almost spans the basin with a length about 2100 kilometers, moisturizes the ambient oasis with numerous rivers and lakes.
中国最长的内陆河——塔里木河，长约2100公里，几乎横贯盆地，与众多的河流湖泊一起滋润著盆地四周的绿洲。
4·However, the natural vegetation will be affected after the implementation of river training works of Tarim river main stem.
塔里木河干流治理工程实施后，将对天然植被的生境产生一系列的影响。
5·In the general, the natural vegetation area of the lower reaches of Tarim River continues decrease, the desertification area goes on increasing, the ecological environment deteriorates gradually.
从总体分析，塔里木河下游自然植被面积持续减少，沙漠化面积继续增加，生态环境日趋恶化。
1·Many of our basin, a large basin with Sichuan basin, Tarim and Junggar basin and Qaidam basin.
我国盆地很多，其中大盆地有四川盆地、塔里木盆地、准噶尔盆地和柴达木盆地。
2·Taking Luntai fault belt of northern Tarim uplift as an example, the main negative inversion phase of the fault may be Suwiyi-Jidike epoch of Miocene, and the inversion ratio is 0.85~0.98.
对塔里木盆地北部隆起轮台断裂带进行的实例分析表明，轮台负反转断裂主反转期为中新世苏维依期一吉迪克期，反转率为0．85～0．98。