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When you look east, west, or south, you can see the snow-covered Tianshan Mountains.

当你向东看,西看或是向南看时,你都会看到被雪覆盖着的天山山脉。

I have to get up before sunup to retrieve the river water that will flow to the east.

直白的翻译呢是我必须在日出前起床来挽回那东去的江水,由一江春水向东流想到的。

North facing openings (and south facing ones above the tropic of Capricorn) receive higher angle sun and therefore require narrower overhead shading devices than east or west facing openings.

北向敞开的地方(和赤道回归线以上的南向)接收来自高角度的太阳光,所以它比东向和西向敞开的地方相比需要较窄小的上部遮阳设备。

Most of China's rivers flow from west to east into the Pacific Ocean except a few in southwest China that flow to the south.

中国的河流除西南部有几条向南流以外,多数是由西向东流入太平洋。

The lithospheric mantle of the Chinese continent, as a whole, is in compressive tectonic regime. 2. The lithosphere of eastern portion of the Chinese continent, being in extensional regime for level-shallow and motion eastward but westward dipping imbricated subduction that formed by high- and lower velocity slabs within lithosphere, suggests that it is in compressional regime in deep levels as a whole.

岩石圈大地水准面异常、水平应力场和P波地震层析等显示,中国东部岩石圈浅层次向东运动,处于相对伸展状态,而深层次高、低速板片向西叠瓦式俯冲形成挤压构造背景,以部分脱耦形式实现不同深度层次之间的调节。

In this area seven microfacies in the Chuangde Fm. red beds can be separated. They are: 1 reddish foraminifera grainstone; 2 reddish microfossils packstone/wackestone; 3 reddish marlstone with microfossils; 4 reddish marlstone; 5 red to variegated floatstone ; 6 reddish shales; 7 reddish radiolarite/ radiolarian chert.In the Yamudok Cuo area, it can be distinguished six microfacies in the redbeds including 1 reddish foraminifera grainstone; 2 reddish microfossils marlstone; 3 reddish shales; 4 yellow-grayish floatstone ; 5 reddish radiolarian chert; 6 reddish chert with radiolaria. The depositional environment of the Chuangde formation can be interpreted from sediments composition, as is deep oceanic basin adjacent to continental slope/rise. The slope/rise setting is indicated by the occurrence of olistoliths and slumped pelagic/hemipelagic limestone, present near the top of the Chuangde Fm.

进一步资料对比研究表明,全球上白垩统海相红层具有以下特征:a上白垩统红层出现在北大西洋、阿尔卑斯、喀尔巴阡、土耳其,向东一直到特提斯喜马拉雅地区和澳大利亚西北角的Exmouth海底高原,横贯整个特提斯和北大西洋;b沉积环境以外陆棚-斜坡和盆地为主,在斜坡环境下多发育有浊流沉积,如Scaglia Rossa和Nietrental组;c有机碳含量普遍很低,0~0.3%之间;d盆地相仅发育红色泥质岩,而斜坡和远洋环境下不仅发育红色页岩,同时还有红色泥灰岩、红色灰岩和红色硅质岩;e北大西洋和地中海地区在Cenomanian-Turonian界线黑色页岩之后不久的Turonian早期就出现红色沉积,而藏南出现在Santonian早期,Exmouth出现在Campanian早期,红层出现似乎有&西早东晚&的趋势。

The fault is zone of sluicing of atmospheric infiltration water flowing from basin west margin to east and sedimentary compaction water flowing from Qija Gulong depression to west.

并且是盆地西缘大气渗入水向东流动及齐家—古龙坳陷沉积压实水向西流动的共同泄水带。

He pointed out that the Chinese were shifting forces eastward in the central area around Tokchon and Yongwon, and sideslipping forces westward from Chosin to the same area, the weakest part of the Eighth Amry line.

他指出,中国人正在向东调动部队、进入德川、宁远地区,并从长津向同一地区转移兵力,该地区是第8集团军战线上最薄弱的地段。

The shortening amount,ratio, rate of of Wuboer area is 32km,40.2%,7.17mm/a,respectively.(3) The Kuzigongsu fault subsidence has several asymmetric half-graben depressions from west to east.These half grabens are characteristic of west-faulting and east-overlapping.According to this phenomenon,the source of the sediments may be mainly from "Wulagen Uplift" to the west when the basin formed.

3认为库孜贡苏断陷盆地自西向东发育多个不对称的侏罗纪箕状断陷,断陷结构为西断东超,说明该盆地形成时主要物源来自于西部的&乌拉根隆起&,由此揭示了南天山西段冲断带东西部分古生界分布差异性的原因。

A hook-shaped peninsula of southeast Massachusetts extending east and north into the Atlantic Ocean.

科德美国马萨诸塞州东南的钩状半岛,向东向北伸入大西洋。

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