查询词典 Tarim Basin

T-WRAS can be used to analyze the conflux process of three headstreams, to evaluate quality, quantity, utilization and synthesize status of water resources in the Tarim River Basin.

该系统可对三源流汇流过程进行分析，对研究区进行数量、质量、开发利用及综合评价，评价结果以图、文、表等多种形式表达。

A Statistical DownScaling Model is used to downscale the output of GCMs in the Tarim River basin. In this paper, maximum temperature and minimum temperature are selected as the predictands.

利用统计降尺度模型SDSM对塔里木河流域未来最高气温和最低气温变化趋势进行分析。

The Kuche Basin, located between the Tianshan intracontinental orogenic belt and the Tarim plate, Xinjiang Uygur Autonomous Region, northwest China, is the tectonic element in the Mesozoic-Cenozoic time, and belongs to a new type of intracontinental flexural basin in the classification of the basin.

库车盆地位于天山陆内造山带与塔里木板块之间，是中新生代发育的构造单元，在盆地分类上属于一种新的陆内挠曲盆地。

Tarim developed into a backarc basin of Laurasia in the splitting of Pangia.

泛大陆的裂解过程中，塔里木地块成为北方劳亚古陆的边缘弧后盆地。

Chagan sag is a secondary tectonic unit in Chagandelesu Depression, northeastern Yingen-Ejinaqi basin, and the basement of the basin is a Paleozoic fold belt of continental margin or island arc at the connection region of North China plate* Tarim plate and Kazakstan plate, with the character of erogenic belt.

查干凹陷属于银根—额济纳旗盆地东北端查干德勒苏坳陷内的一个次级构造单元，其盆地基底为古生代时期华北板块、哈萨克斯坦板块和塔里木板块交接部位形成的陆缘或岛弧褶皱带，具有古生代造山带的性质。

This paper summarizes various structural models, structural belts, Cenozoic deformation frameworks and tectonic evolution concerning intraplate deformation in the West Kunlun - Pamir Cenozoic erogenic belt and Southwest Tarim foreland basin and suggests that the Cenozoic intraplate deformation be characterized by segmentation and stage evolution.

笔者总结了西昆仑—帕米尔造山带及塔西南前陆盆地板内变形的各类构造模式、构造分带、新生代变形格局及构造演化，提出其新生代板内变形具有弧形构造分段性和阶段性演化的特点，发现了依格孜牙、柯克亚、桑株—杜瓦、卡兹克—阿尔特薄皮弧形推覆构造、齐姆根主弧形构造段及玉力群—克里阳构造段的三角带构造及叶尔羌—棋盘对冲过渡型弧形构造。

In the Middle and Late Cambrian, similar to the lithofacies palaeogeographic pattern of the Early Cambrian, the land area was gradually reduced, the basin area was enlarged, while the Tarim carbonate platform changed little.

中寒武世和晚寒武世的岩相古地理格局与早寒武世相似，但陆地面积逐渐缩小，盆地面积逐渐扩大，塔里木碳酸盐岩台地变化不大。

After interpreting natural earthquakes since 1953,the author also did a exploratory research on the lithospheric tectonic relationship of South Tienshan orogen,and considered in west and east side,West Kunlun orogen and Tafim block,and considered that Tarim block subducts beneath the West Kunlun orogen and South Tienshan orogen in two direction;In Pamir area,a syntaxis formed with the West Kunlun orogen obducts upon the South Tienshan orogen,and result in the two great orogens that rejuvenated during Cenozoic and the subduction and jointing relationship of the two orogens and Tarim block,showing a specific basin-and-range coupling system.

5通过对天然地震剖面的解释，探索了南天山造山带、西昆仑造山带和塔里木地块的岩石圈大地构造关系，认为在东西两侧，塔里木地块为南北直接俯冲于西昆仑造山带和南天山造山带之下的双向俯冲模式；在中部地区，西昆仑造山带在帕米尔地区形成构造结并仰冲于南天山造山带的前陆冲断带之上，形成了两个新生代复活的巨型造山带，以及两大造山带与塔里木地块之间的俯冲和对接关系，形成了独特的&盆一山&耦合体系

In author's opinion, it had taken place back-arc foreland thrust belt during Triassic abased on the S-D peripheral foreland basin thrust nappe in South-eastern Tarim depression and Southern Tarim uplift, which made of a series of nappes and fault-related folds from south to north.

初步提出盆地南缘在志留—泥盆纪周缘前陆冲断系的基础上发育三叠纪古弧后前陆冲断带。它位于现今塔里木盆地的东南坳陷和塔南隆起地区，由一系列自盆地南部边缘向盆地内部叠瓦冲断的逆断层及相关褶皱组成的复杂冲断构造。

In the west, there are some obvious high velocity regions, such as tectonically stabe Tarim, Junggar, Turpan, Hami basin and east of Qaidam basin, Sichuan basin and to its south, Taiwan Strait and so on. High velocities also exist in Erdos.

在中国西部，构造上相对稳定的塔里木盆地、准噶尔盆地和吐鲁番-哈密盆地，以及柴达木盆地东端、四川盆地及其南部地区，台湾海峡等是明显的高Sn速度区，鄂尔多斯地台也偏高。

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。