English translation for "右行"

[ yòuháng ]
a surname 短语和例子

Related Translations:

右右: usuke

右: Ⅰ名词1.(面向南时靠西的一边) the right side; the right 短语和例子靠右走 keep to the right; 向右拐弯 turn to the right2.(西) west 短语和例子山右 areas west of the taihang mountains, specifically shanxi province3.[书面语] (地位

Example Sentences:

	1.	And if you go in , should you turn left or right 若你毅然向前，那是要左转还是右行？
	2.	I : use of props , space : suspended props menu display status , left bank counterclockwise trip right choice props clockwise choice props I :使用道具, space :暂停,道具菜单显示状态时,左行a逆时针选择道具右行d顺时针选择道具
	3.	Take i - 55 to lake shore drive north . exit at wacker drive . stay to very right and go up ramp and proceed to third light , michigan avenue 取道i - 55公路直达湖岸车道北，从沃克车道驶出，一直右行上坡，第三个红绿灯处直走进到密西根大道。
	4.	If you are coming from the north by car , take i - 94 edens expressway to i - 90 kennedy expressway and stay with it as it turns into i - 94 dan ryan expressway . continue south on i - 94 and keep to the right 取道i - 94号伊甸园高速路到i - 90号肯尼迪高速路，一直朝前，在同i - 94号丹莱恩高速路交汇处上i - 94号路向南走，一进右行。
	5.	On the basis of detailed field work and structural analysis , this paper presents a new geometrical and kinematic data that reveal the staictural characteristics of qinglong fault zone . this fault zone is composed of numerical ew faults with an arrangement of dextral step pattern in the western part , and consists of maquanzi - datun fault and tumenzi - mingshui fault in the eastern part 本文通过较为详细的野外调查和室内研究，并结合前人的研究资料，以构造解析为指导思想，对断裂带的几何学、运动学特征进行了研究：青龙断裂带是由一系列近东西向的断层组合而成，断裂带西段呈明显的右行右列式分布，东段主要有马圈子?大屯断裂和土门子?明水断裂组成。
	6.	The fault controlled the magmatism and metallization relevant to the contact zone , and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene . the fault zone deformed right - laterally under ne - sw striking transtention , and new joints zone was produced at the end of the two main faults because of local stress concentration . the fault produced inchoative cataclastic rocks , and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks , which was during the himalayan movement 其后的继承性活动在断裂带内形成碎裂程度最强达到碎裂岩的碎裂岩系列构造岩，变形带两侧发育两组典型的共轭剪节理；第二次在晚白垩世?始新世，断裂在北东?南西向近水平挤压作用下右行张扭性活动，断裂带两主断裂在斜列重叠的端部由于局部应力集中进一步扩展形成节理带，而断裂在岩体区也发育两组典型的共轭剪节理，断裂内形成初碎裂岩为主的构造岩；第三次是喜山期以西侧抬升、东侧下降的强烈升降为主的活动，在基岩中，主断层两侧围岩出现微破裂。
	7.	The study on the structural feature opened out by the non - seismic ( mt ) profile of xiaonangou in qinglong mountain on the west edge of ordos basin and the seismic profile across helan mountain shows that a series of thrust blocks - qinglong - luoshan - nioushou - helan mountain , were the thin - skin structure formed by the westward compression of ordos block and the dextral shear of alashan block 通过对盆地西缘青龙山南端小南沟的非地震mt剖面以及横穿贺兰山的地震剖面揭示的构造形态研究认为，盆地西缘一系列推覆体青龙山?罗山?牛首山以至贺兰山是由于鄂尔多斯地块向西推挤同时与阿拉善地块的右行运动所产生的“薄皮构造” 。
	8.	Alkali basite , which came from upper mantle or lower crust , invaded through those structure , which not only bring cu et al mineralizing elements , but also the most important is that thermal energy . it cycled the formation water ( yinmin fonnation and luoxue formation ) , and form alkali - rich , middle - high temperature and salinity fluid mixed with alkali - rich magmatic water . there were high rate of percolation and well voidage in the contact zone between yinmin purple stratum and yinmin rubblerocks , which is in favor of the transposition and mineralization of minerogenetic fluids 因此，总结东川稀矿山式铜矿成矿模式为沉积( fe 、 cu ) ?热液叠加( cu )改造：晋宁-澄江期，小江深大断裂发生走滑运动，在东川矿区造成右行旋扭及其派生构造，形成“ z ”字形落因破碎带，同时来自深源(下地壳或上地幔)碱基性岩浆侵入，不仅带来了大量cu等成矿物质，更重要的是提供了热源，促使地层水(落雪组白云岩和因民组紫色层)循环，与富碱( na和k )岩浆水混合，形成富碱中高温高盐度流体。
	9.	D ) the invasion of jinningian - chengjiangian alkali basite were unambiguous , the distribution of those rocks form " z " in shape , which similar with luoyin fracture zone and the distribution of copper deposit . it shows that copper deposits were controlled by discordogenic fault and its derived sub - structure , and there are relationship between copper deposit and jinningian - chengjiangian alkali basite . e ) most of minerogenetic age of copper deposit , which located in kunyang rift valley , belongs to jinningian - chengjiangian ( between 900 - 650ma ) , similar with the time limit of breaking - up of rodinia 东川矿区晋宁-澄江期碱基性岩侵入活动明显，常作为因民组复杂角砾岩胶结物和岩脉(体)产出，多分布于深大断裂及其派生的次级构造附近，明显受南北向小江深大断裂走滑运动引起的右行旋扭及其派生构造控制，与“落因破碎带”和“铜矿分布”较吻合，均为“ z ”字形。

Similar Words：: "右型大动脉转位" English translation, "右型大血管转位" English translation, "右型高半胱氨酸" English translation, "右型完全性大动脉转位" English translation, "右形" English translation, "右行并合步" English translation, "右行叠绕组" English translation, "右行断层" English translation, "右行诡" English translation, "右行交通" English translation