查询词典 Tarim

Institute of Plant Science and Technology, Tarim University Alar, Xinjiang 843300

塔里木大学植物科技学院，新疆阿拉尔 843300

College of Animal Science and Teehnology, Tarim University, Alar, Xinjiang 843300

塔里木大学植物科技学院，新疆阿拉尔843300 [2]塔里木大学动物科技学院，新疆阿拉尔843300

Institute of Xiyu Culture, Tarim University, Alar , Xinjiang 843300

塔里木大学西域文化研究所，新疆阿拉尔 843300

Regarding the xinjiang frontier trade development shallow Blaker,(the tarim university institute of economics and management, xinjiang alar 843300) Abstract: border trade in border areas neighboring countries as a special form of international trade, and to promote the border areas of economic and social development, accelerate the development of international economic resources and has a special meaning.

关于新疆边境贸易发展的浅析张强（塔里木大学经济与管理学院新疆阿拉尔 843300）摘要：边境贸易作为毗邻国家边境地区的一种特殊的国际贸易形式，对于促进边境地区的经济和社会发展，加快国际经济资源的开发与移动有着特殊的意义。

Based on surface and subsurface geological data, combined with achievements about the west Kunlun orogen, Tibet, Tarim basin and Altun tectonic zone, it is analysed that geometry and kinematics of the west Kunlun fold-thrust-belt between Sangzhu country in the west and Cele county in the east.

本文通过对研究区地面地质资料和地下地质资料的分析，并结合西昆仑造山带、青藏高原、塔里木盆地和阿尔金构造带研究的新进展，对西昆仑北缘冲断带桑株—策勒段的构造形态和演化历史作了深入的剖析与探讨，取得了一些新认识。

Lop Nur is now the lowest in the north, one of the biggest depression that was once a center of stagnant water in the Tarim Basin, originated in ancient Tianshan, the Kunlun Mountains and the Altun Mountain watershed, stream into Norbu depressions formed lakes.

现在罗布泊是位于北面最低、最大的一个洼地，曾经是塔里木盆地的积水中心，古代发源于天山、昆仑山和阿尔金山的流域，源源注入罗布洼地形成湖泊。

The Tumxuk fault zone in the western Tarim Basin is a boundary between the Bachu Fault-Uplift,a sub-order unit of the Central Rise whose predecessor was a Jinningian collisional orogen,and the Awat Sag(sub-order unit of the North Depression).

塔里木盆地西部的吐木休克断裂带是中央隆起(前身是晋宁期碰撞造山带)的次级单元巴楚断隆与北部坳陷的次级单元阿瓦提凹陷之间的分界。

Synthetic analyses based largely on the platform/inner shelf trilobite faunas suggest that the Chinese eastern Peri-Gondwanan plates and terranes may have belonged to a single biogeographic province during the Tremadocian and the late Katian-Hirnantian, but may be divided into two sub-provinces during the Floian-early Katian (Arenig-Caradoc): One consists of South China, Tarim and Annamia, and the other may include North China, Sibumasu, southern Tibet, Tianshan-Beishan and possibly Hainan.

对这些属于东泛冈瓦纳的中国区块的台地或内陆棚三叶虫动物群的综合分析研究证明，它们在特马豆克期以及凯迪晚期－赫南特期(late Katian-Hirnantian)或阿石极期应归属同一生物地理区，而在弗洛期－凯迪早期(Floian-early Katian)或阿仑尼克期－卡拉多克期(Arenig-Caradoc)则可划分为两个生物地理亚区：一个由华南、塔里木板块和安南或印支地体组成，另一个包括华北板块以及滇缅马、藏南、中天山－北山地体。

Keywords Carbonate reservoir;Karst reservoir;Fractured and caverned reservoir;Oil and gas exploration;Exploration technology;Development technology;Tahe Field;Tarim Basin

碳酸盐岩油气藏；岩溶油气藏；缝洞型油气藏；油气藏勘探；勘探技术；开发技术；塔河油田；塔里木盆地

There are two branches stretched into China from Tethys during Cenomanian–Turonian in the Cretaceous, including the south branch, where occurred OAE2 in the Tibetan region, and north branch, where existed OAE2 in the southwestern of Tarim Basin too, thus it provided another evidence for OAE2's globality.

白垩纪Cenomanian-Turonian时期古特提斯海伸向我国的南北两个分支，其南支在西藏地区存在OAE2大洋缺氧事件，而北支在塔里木盆地西部也存在OAE2事件，这对丰富我国白垩纪事件研究、进行全球白垩纪OAE2大洋缺氧事件对比及其成因机制的探讨、查清塔里木盆地白垩纪古环境和烃源岩大规模形成的古气候控制因素以及白垩纪海相生物群演化、更替及其与重大地质事件的联系等具重要意义。

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。