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Home > english-chinese > "龙门山" in Chinese

Chinese translation for "龙门山"

longmen shan

Related Translations:
龙门:  gantrygoal keeperlong menlong monlongmenportal shapedryongmunryumontatsukadoyong mum
龙门所:  longmensuo
龙门石窟:  the longmen grottoes (in luoyang)
龙门路:  lung mun road
龙门场:  longmenchang
龙门桅:  pair maststwin masts
石龙门:  bau
龙门溶洞:  ryongmun cavern
霍龙门:  huolongmen
起重龙门:  gantry
Example Sentences:
1.Longmen mountain a cool world
龙门山里话清凉
2.In ancient myths , every spring thousands of carps come to the dragon door hoping that they can jump over it
古代神话传说:每年春季有鲤鱼数干前赴龙门山下,但是多数不能跳越。
3.4 ) analyses boundary faults of the cenozoic longmenshan foreland basin , and thinks the basin boundary faults , being active fault , are thrust and dextral strike - slip . so the longmenshan foreland basin is dextral strike - slip foreland basin
4 )通过对新生代龙门山前陆盆地边界断裂的考察分析,认为盆地边界断裂具逆冲推覆及右旋走滑作用特点,为活动断裂。
4.In the end , i discussed the formation and evolution character of long sequence cycles , which had close relation to asynchronous thrust action of longmen mountains and micang - daba mountains
详细讨论了短期、中期和长期旋回层序的结构类型、沉积序列、叠加样式和分布模式,最后探讨了长期旋回层序的形成、演化特征以及与龙门山和米仓山?大巴山两构造带非同步逆冲推覆作用的关系。
5.Abstract : this paper describes in detail the structural characteristics of the taiansi - gangou - cangping fault macroscopically and microscopically , and distinguishes the fault is the main slip ( decollement ) plane in the middle and southern sector of the frontal nappe belt in longmen mountains
文摘:泰安寺-干沟-苍坪断裂是龙门山前缘推覆构造带中南段主滑面,文章详细描述了该断裂在宏观和微观上的构造变形特征。
6.According to the analysis of newly - compiled 1 : 2000000 gravity and magnetic data , there exist three ( eastern , central and western ) deep tectonic areas in northern china , which are hounded in the east by helan mountain - liupan mountain - longmen mountain line and in the west by xingxingxia - ruoqiang line
摘要根据新编制的1 : 200万重磁资料分析,中国北部深层存在东、中、西3个构造区,其东界在贺兰山六盘山龙门山一线,西界在星星峡若羌一线。
7.At the same time , attained following fruits : 1 . the tectonic analysis indicated that the distortion of the foreland basin was mainly attributed to the movements of longmen mountains , the structural features , forming periods , and transformation fashions are different between the northern and southern segments
主要取得如下成果: 1 、构造研究表明川西坳陷形成与形变主要受控于龙门山造山带,表现为坳陷内部南、北段构造特征、形成期及其变形方式上的差异。
8.The frontal structure of longmenshan in the west of sichuan is very complex , showing intense structure deformation in overthrust belt , high structure amplitude , steep stratigraphic dip , developed fault blocks , complex seismic wave field , frequent change of lateral velocity , and poor image of post - stack time migration processing
摘要川西龙门山前缘构造非常复杂,逆掩推覆构造带构造形变强烈,构造幅度大,地层倾角陡,断块发育,地震波场复杂,速度横向变化大,常规叠后时间偏移处理成像效果较差。
9.2 ) analyses and researches systematicly the lithofacies , sedimentary facies and depositional environment of the dayi conglomerate in the cenozoic longmenshan foreland basin . this paper analyzes detailed six coarse elastics lithofacies , five mid - elastics lithofacies and three fine elastics lithofacies . establishes the association of three depositional environment types including alluvial fan and river
2 )对新生代龙门山前陆盆地大邑砾岩岩相、沉积相和沉积环境进行了系统分析和研究,划分出6种粗碎屑岩相、 5种中碎屑岩相、 3种细碎屑岩相,确定了大邑砾岩为冲积扇相、河流相沉积环境的组合。
10.In the early xujiahe age ( t3x2 3 ) , micang - daba mountains were still in stable uplift station with low amplitude . on the contrary , the thrust action of longmen mountains was active . at this age , the northeast sichuan foreland basin was mainly influenced by remote effect of longmen mountai ns " thrust action
认为在须家河早期( t _ 2x ~ ( 2 - 3 ) ) ,米仓山?大巴山构造山系尚处于低幅稳定隆升状态,而龙门山构造山系的逆冲推覆作用较为活跃,川东北前陆盆地主要受龙门山逆冲推覆作用的远端效应的作用为主。
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