查询词典 the rather that

Who would these fardels bear, To grunt and sweat under a weary life, But that the dread of something after death - The undiscover'd country, from whose bourn No traveller returns - puzzles the will, And makes us rather bear those ills we have Than fly to others that we know not of?

谁愿意负着这样的重担，在烦劳的生命的压迫下呻吟流汗，倘不是因为惧怕那不可知的死后，惧怕那从来不曾有一个旅人回来过的神秘之国，是它迷惑了我们的意志，使我们宁愿忍受目前的磨难，而不敢逃到我们所不曾知道的地方？

Who would fardels bear, To grunt and sweat under a weary life, But that the dread of something after death, The undiscover'd country from whose bourn No traveler returns, puzzles the will, And makes us rather bear those ills we have Than fly to others that we know not of?

谁也不甘心，呻吟、流汗拖着这残生，可是对死后又感觉到恐惧，又从来没有任何人从死亡的国土里回来，因此动摇了，宁愿忍受着目前的苦难而不愿投奔向另一种苦难。

Who would these fardels bear, To grunt and sweat under a weary life, But that the dread of something after death- The undiscover'd country, from whose bourn No traveller returns- puzzles the will, And makes us rather bear those ills we have Than fly to others that we know not of?

谁也不甘心，呻吟、流汗拖着这残生，可是对死后又感觉到恐惧，又从来没有任何人从死亡的国土里回来，因此动摇了，宁愿忍受着目前的苦难而不愿投奔向另一种苦难。

Who would fardels bear, To grunt and sweat under a weary life, But that the dread of something after death, The undiscover'd country from whose bourn No traveller returns, puzzles the will And makes us rather bear those ills we have Than fly to others that we know not of?

谁甘心挑担子，拖着疲累的生命，呻吟，流汗，要不是怕一死就去了没有人回来的那个从未发现的国土，怕那边还不知会怎样，因此意志动摇了，因此便宁愿忍受目前的灾殃，而不愿投奔另一些未知的昔难？

Who would fardels bear, To grunt and sweat under a weary life, But that the dread of something after death, The undiscover'd country from whose bourn No traveler returns, puzzles the will, And makes us rather bear those ills we have Than fly to others that we know not of?

谁会fardels 负担，作古噜声和冒汗在疲倦的寿命，但那之下某事的忌惮在死亡以后， undiscover'd 国家从bourn 没有记录回来，困惑意愿，和使我们宁可负担那些不适我们有比飞行对其他人我们知道不是？

Who would these fardels bear, To grunt and sweat under a weary life, But that the dread of something after death- The undiscover'd country, from whose bourn No traveller returns- puzzles the will, And makes us rather bear those ills we have Than fly to others that we know not of?

但他自己只要用把尖刀就能解脱了。谁也不甘心，呻吟、流汗拖着这残生，可是对死后又感觉到恐惧，又从来没有任何人从死亡的国土里回来，因此动摇了，宁愿忍受着目前的苦难而不愿投奔向另一种苦难。

Note that most fatalists tend to stay away from social situations, even if they are involved somehow, as they prefer to speculate and watch the scenario through to the conclusion rather than influence or that they will not have any effect due to believing they lack something as a person.

要注意多数死亡主义者往往远离社交情景，即便他们有所参与，因为他们更愿意揣测，看着情景进行一直到结束，而不是去影响，或者，因为他们认为自己缺乏作为一名人类来说的某样东西，从而不会产生。。。任何的影响。

However, invertors might not understand employee bonus that should be treated as expense in the income statement, rather than as a distribution of earnings in the statement of retained earnings at the beginning. Accordingly, investors did not consider the factor of director compensation and employee bonus in their investment decision-making so that there had been existence of mechanical hypothesis on employee bonus.

但是在未修改法规之前，投资人并未了解员工分红应该列为损益表中的费用，而是认为列在保留盈余中作为盈余之分配，因此投资人在进行投资决策时未能考虑董监酬劳以及员工分红，所以投资人对员工分红会存在机械性假说之状况。

As she came down the stairs rather hurriedly and embarrassedly, as the state of spirit of her character was supposed to be that at that point, she was wearing a beautiful lavender-coloured dress with the back part open until her mid-back, she had her hair down in soft curls, simple make up, a small handbag and a cute little silver necklace.

她匆忙而窘迫地走下楼梯，因为此时她角色的心理状态理应如此。她身着一件淡紫色半露背的连衣裙，头发松微微卷曲，淡妆，手持串珠小包，配戴了一条漂亮的银项链。

Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

根据Ar-Ar热年代学研究，精确测定了早二叠世伸展变形和晚二叠世挤压变形的峰期时代分别为290Ma和259Ma.2、提出了关于哈尔里克山南麓小铺一带变质带和变质作用的新认识根据显微观察资料和特征变质矿物的出现，把小铺一带的变质岩由SW向NE方向依次划分为黑云母带、石榴石带、十字石带、红柱石带和矽线石带等变质带；初步确定该区的变质作用属于中温-低压型，变质作用发生的时代为290Ma左右，是该区早二叠世地壳伸展的产物。3、首次提出哈尔里克山南麓在石炭纪可能发育弧后盆地的新观点根据哈尔里克山南麓原&居里得能组&岩屑砂岩的碎屑锆石SHRIMP U-Pb定年，确认这套地层的沉积不早于晚泥盆世，很可能是石炭纪，而不是前人所说的前寒武纪；结合对其区域地质背景、源区位置和沉积环境分析，推测该区石炭纪可能为滞后弧后盆地和弧后隆起区构造背景。4、进一步证明哈尔里克山不发育与岛弧演化相关的泥盆纪岩浆活动根据对代表性闪长岩和花岗岩的锆石SHRIMP年代学研究获得的新资料，结合该区已有相关资料的综合研究，确定哈尔里克山岩浆岩分别形成于奥陶纪-志留纪和石炭纪晚期-二叠纪，不存在泥盆纪的岩浆岩，进而认为该区泥盆纪不属于岛弧环境。5、重建了哈尔里克山古生代以来的地质演化过程根据区域资料以及本次研究所获得的资料，把哈尔里克山古生代以来的构造演化划分中奥陶世-早志留世为岛弧、中志留世-晚泥盆世为弧后区、石炭纪弧后伸展、二叠纪为后碰撞伸展与挤压、中生代差异隆升和晚新生代陆内再造山过程等构造阶段。6、初步估算了哈尔里克山地壳缩短率和缩短量根据前中生代地层褶皱估算的哈尔里克山南山口-口门子、石城子-白石头和沁城-小铺三条剖面的地壳缩短率分别为16.2%、19.8%和20.1%，相应的地壳缩短量分别为4.3km、9km和11.3km。

And Pharaoh spoke to Joseph, saying, Your father and your brothers have come to you.

47：5 法老对约瑟说，你父亲和你弟兄们到你这里来了。

Additionally, the approximate flattening of surface strip using lines linking midpoints on perpendicular lines between geodesic curves and the unconditional extreme value method are discussed.

提出了用测地线方程、曲面上两点间短程线来计算膜结构曲面测地线的方法，同时，采用测地线间垂线的中点连线和用无约束极值法进行空间条状曲面近似展开的分析。