乌苏

Our territory for the four-terminal : in the most eastern Heilongjiang and Wusuli the centerline of the main channel of the intersection (135 ° E), an the most western end near the Pamirs (73 ?E), things are about 5,000 km. in the south Cengmuansha (4 ?N), the most northern end of Mohe in the north of the main channel of the Heilongjiang Center Line (53 ?N), North and the South are about 5,500 km.

我国领土的四端为：最东端在黑龙江和乌苏里江的主航道中心线的相交处（135篍多），最西端在帕米尔高原附近（73篍），东西相距约5000千米，南端在曾母暗沙（4篘）、最北端在漠河以北黑龙江主航道的中心线上（53篘）多，南北相距约5500千米。

Zhenbao is an island in the Ussuri River, which demarcates the Sino-Russian border.

珍宝岛是乌苏里江中的岛屿，其中划定的中俄边界。

The action potentials and the calcium current in single cardiac myocyte were recorded with whole cell patch clamp recording techniques.

3～ 30 μmol·L- 1 的高浓度可诱发异常节律。乌苏里藜芦生物碱对心肌细胞钙电流有促进作用，此作用呈短暂的浓度依赖性增强。

According to the agreement to be signed, Russia will return Yinlong Island and half of Heixiazi Island.

根据签署的协议，俄国将归还银龙岛和半个黑瞎子岛，这两个岛地处黑龙江和乌苏里江的会聚地，因此两国的自然分界。

According to the agreement to be signed, Russia will return Yinlong Island and half of Heixiazi Island.

根据即将签署的协议，俄方将归还位于黑龙江和乌苏里江交汇处的银龙岛和一半的黑瞎子岛，这两岛一直作为两国的天然边界。

The company had a big outstanding talent to start an undertaking the team, the success has prepared for construction the Xinjiang Wusu 1,000,000 tons iron and steel plants and the Ruyang Yabin mining industry lead zinc mining project.

公司拥有一大优秀人才创业团队，成功筹建了新疆乌苏100万吨钢铁厂和汝阳亚宾矿业铅锌开采项目。

Hereby it seems that the megainterstadial climates of the Salawusu valley at least went through ten wet-warm events and nine cold-dry events and could be divided into five substages: MIS3e (58.85~48.98 ka BP), MIS3d (48.98~39.55 ka BP), MIS3c (39.55~34.59 ka BP), MIS3b (34.59~26.47 ka BP) and MIS3a (26.47~23.07 ka BP).

据此，末次间冰阶萨拉乌苏河流域至少经历了10次温湿和9次冷干气候波动，且可划分为MIS3e(58.85~48.98kaBP)、MIS3d(48.98~39.55kaBP)、MIS3c(39.55~34.59kaBP)、MIS3b(34.59~26.47kaBP)和MIS3a(26.47~23.07kaBP)等5个亚段。

Ussuri名叫雅巴沙local white salmon, rabbit fish.

乌苏里白鲑地方名叫雅巴沙、兔子鱼。

It also suggested that the climate and environment in the area are characterized by changeability, sensitivity, instability, its general changes are the positive process of desertification correspondingly to the dry-cold steppe or desert steppe and desert, while the reverse process correspondingly to warm semi-humid forest steppe and temperate-humid shrub steppe.

进一步证实了古土壤S〓发育和河湖相沉积的萨拉乌苏组堆积时为温暖半湿润的森林或森林草原环境，全新世的砂质古土壤或湖沼相沉积时为温湿灌丛草原或疏林草原环境，黄土沉积时为半干旱干草原环境，风成砂沉积时为干旱荒漠草原甚至荒漠环境。

We have observed the structure of these dune sands and analyzed the grain-size,surface textural features and several main chemical elements of them,the results showed that:(1) these dune sands have some eolian structure characteristics which are similar to the recent dune sands;(2) they are also similar to the recent dune sands in grain-size components,and parameters of Mz,?滓,Sk and Kg,as well as in several main chemical components;(3) the scatter plots of Mz-?滓,SiO2-Al2O3+TOFE and the probability curves of grain-size showed that these paleo dune sands are different from paleosols and fluvio-lacustrine facies but are consistency with recent dune sands;and(4) the quartz sands have well roundness and some surface textural features such as dish-shape pits,crescent-shape pits,pockmarked pits,upturned cleavage plates,siliceous precipitates and siliceous crevasses,indicating that they had been carried for a long time by the wind.

对这些沙丘砂的沉积构造观察以及粒度、扫描电镜和常量化学元素分析结果表明：(1)这些沙丘砂具有与现代沙丘砂相似的风成沉积构造特征；(2)粒度及其参数--Mz、σ、Sk和Kg，以及主要化学组分SiO2、Al2O3和TOFE也与现代沙丘砂相近；(3)Mz-σ、SiO2-Al2O3+TOFE散点图和概率累积曲线显示这些沙丘砂与萨拉乌苏组中的河湖相、古土壤差别明显，而与现代沙丘砂一致；(4)石英砂颗粒具有良好的磨圆以及碟形坑、新月形坑、麻坑、上翻解理薄片、硅质沉淀和硅质裂纹等表面结构特征，反映其曾受持久的风力搬运作用。

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。