orogeny中文是什么意思

• n.
  【地质学；地理学】造山运动，造山作用。
  亦 -genesis , -genic, -netic adj.
  

• a alachian orogeny    阿帕拉契亚造山运动
• a yntian orogeny    阿森特造山运动
• acadian orogeny    阿卡德造山运动; 阿卡迪亚造山运动; 阿卡迪造山; 阿克殿造山运动
• aedennian orogeny    阿登造山运动
• agassiz orogeny    阿格赛兹造山运动
• algoman orogeny    阿尔戈马造山运动; 阿尔网纹造山运动
• alleghenian orogeny    阿莱干尼造山运动; 阿利根尼造山幕
• allegheny orogeny    阿勒格尼造山运动
• alpine orogeny    阿尔卑斯式高山造山作用; 阿尔卑斯造山运动
• alpineage orogeny    阿尔卑斯期造山运动
• alpinehimalayantype orogeny    阿尔卑斯喜马拉雅型造山运动
• alpinetype orogeny    阿尔卑斯型造山运动
• alpinotype orogeny    阿尔卑斯型造山酌
• amorican orogeny    阿莫里加造山运动; 阿莫利坎造山运动
• antler orogeny    安特勒造山运动
• appalachian orogeny    阿巴拉契亚造山运动; 阿帕拉契亚造山运动; 阿帕拉契造山运动
• arbuckle orogeny    阿巴克尔造山运动; 阿尔布克尔造山运动
• ardennian orogeny    阿当造山运动; 阿登造山运动
• armorican orogeny    阿莫里克造山运动
• assyntian orogeny    阿森特造山运动
• asturian orogeny    阿斯突里造山运动
• attic orogeny    阿蒂克造山运动
• attican orogeny    阿提克造山运动
• yenshan orogeny    燕山运动
• orogeny (orogenesis)    造山作用
• orogenlic phase    造山运动期

• A general survey of the formation , evolutionary histories of continental orogenic belts both in china and abroad reveals that orogenic belts have often undergone numerous and varied tectono - evolutionary stages , such as palaeocontinental break - up , ocean - land transition , continental matching - collision , intracontinental extension - basin - range coupling , and new tectonic uplift ( intracontinental orogeny ) , which are respectively accompanied by characteristic volcano - magmatisms
  纵观我国以至全球的大陆造山带形成、演化历史，一个造山带往往经历了古大陆裂解、洋陆转换、陆块拼合碰撞、陆内伸展盆山耦合和新构造隆升（陆内造山）等众多不同的构造演化阶段，这些不同的构造演化阶段和不同的构造环境均有特定火山岩浆作用与之相伴。
• Scanning the formation - evolutionary histories of continental orogenic belts in both our country and whole workd , an orogenic belt has often undergone numerous and various tectono - evolutionary stages , such as palaeo - continental break - up , ocean - land transition , continental matching - collision , intracontinental extension - basin - range coupling , new tectonic uplift ( intracontinental orogeny ) , etc . , which are respectively companied with characteristic volcano - magmatism
  纵观我国以至全球的大陆造山带形成-演化历史，一个造山带往往经历了古大陆裂解、洋陆转换、陆块拼合-碰撞、陆内伸展-盆山耦合和新构造隆升（陆内造山）等?多不同的构造演化阶段，这些不同的构造演化阶段和不同的构造环境均有特定火山岩浆作用与之相伴。
• The stratigraphic sequences and sedimentological characteristics indicate that the main body of the bayan har basin is composed of triassic flysch sediments deposited in a foreland basin during the triassic . in the study of jinshajiang orogenic belt , in the applying archipelago theory and particular anatomies to basin analysis in this orogeny , the model of jinshajiang archipelago mountain building and basin building is set up . the orogenic - sedimentology and sedimentary basin analysis system is printed archipelago paleogeography any more
  在金沙江造山带研究中，将多岛弧盆理论应用于这个造山带的沉积盆地分析研究中，对金沙江多岛弧盆造山带进行了详细解剖，建立金沙江多岛弧盆系造山造盆的模式，进一步发展造山带沉积学和沉积盆地分析理论体系。
• The basin has three evolutionary stages including intracontinental rift basin in p1 - p2 , down basin in t2 + 3 - k and the strong trust - orogeny process in n - q . according to the unconformity contact relationship and sedimentary components , santanghu basin is divided into four tectonic sequence such as : o - c tectonic sequence of basement , pi - p3 tectonic sequence , t - k tectonic sequence and n - q tectonic sequence
  根据盆地地层之间的不整合接触关系，考虑到各层序沉积物组成与生物组合特征等因素，将三塘湖盆地划分为： ( o ? c )基底构造层序，二叠系( p )构造层序，三叠系( t ) ?白垩系( k )构造层序和第三系、第四系构造层序。
• Tectonic analysis controlling gold mine mineralization in taihua group suggest that ductile fractures chang into brittle - ductile ones going with upliftling of xiaoqinling area after in - china orogeny . brittle fractures form on the basis of brittle - ductile ones that develop and inherit the characteristic of the latter stress field . folds and faults analysis in taihua group and its bilateral reveal that yanshanian tectonic evolution of xiaoqinling area undergo at least three phases of deformation
  太华群内金矿成矿构造分析表明，印支期碰撞造山后小秦岭挤压抬升，控矿韧性剪切带向脆韧性转化( 207 148ma ) ，在脆韧性剪切带基础上叠加改造形成容矿断裂，脆性断裂的发育继承了韧脆性剪切带发育时的应力场特征。
• The author also suggested that the fuxin block developed on the base of the geosyncline in the huabei craton , and had experienced three period process of orogeny , including hercynian folding orogeny in continental margin , mainly indo - sinian to early yanshanian intracontinental fold - faulting orogeny , and late yanshanian to early himalayaian intracontinental range - basin post orogeny
  认为阜新地块是在克拉通裂陷槽基础上发育起来的，经历了海西期陆缘褶皱始造山、印支?早燕山陆内褶断主造山、晚燕山?早喜马拉雅陆内盆山后(重)造山等过程。
• In the light of tectonic evolution stage and metallogenesis , these metallogenic system ( assemblage ) could be classified as follows : ( 1 ) the pre - divergent metallogenic system in the southwest margin of north china paleocontinent in the archean - meso proterozoic : dongdashan iron , jinchuan nickel - copper . ( 2 ) the divergent metallogenic system in the northern margin of the qaidam paleoplate in the middle - late proterozoic : huashugou - liugouxia iron . ( 3 ) the metallogenic system in the active margin in the early paleozoic : the metallogenic assemblage in the island arc - rift in the early stage ( baiyinchang - qingshuigou copper - polymetallic ) ; the metallogenic assemblage in island arc in the middle - late stage ( honggou - jiaolongzhang copper - polymetallic ) ; the back - arc extensional basin ( zhuzhuiyaba - jiugequan - shijuli copper ) ; the metallogenic assemblage in connection with subduction and magmatic - hydatogenesis ( taergou - xiaoliugou wolfram ; huashugou - liugouxia copper ; dadonggou - diaodaban lead - zinc ) ; the metallogenic assemblage is related to the oceanic crustal shards ( dadaoerji chromite ; yushigou chromite ) . ( 4 ) the metallogenic system has something to do with collision - type orogeny : the metallogenic assemblage in foreland basin ( tianlu copper ) ; the metallogenic assemblage with the intracontinental orogeny and ductile shear ( hanshan - yingzhuishan gold )
  根据构造发展阶段和成矿作用特点，确定本区成矿系统及组合如下： ( 1 )华北板块西南边缘太古宙中元古代裂解期前成矿系统：东大山铁成矿组合，金川镍铜成矿组合； ( 2 )柴达木板块北缘中、新元古代裂解成矿系统：桦树沟柳沟峡铁成矿组合； ( 3 )加里东期活动大陆边缘成矿系统：早期岛弧裂谷成矿组合(白银厂清水沟铜及多金属成矿组合) ，中、晚期岛弧成矿组合(红沟蛟龙掌铜及多金属成矿组合) ，弧后扩张盆地成矿组合(猪咀哑巴九个泉石居里铜及多金属成矿组合) ，与俯冲作用有关的岩浆热液成矿组合(塔尔沟小柳沟钨成矿组合，桦树沟柳沟峡铜成矿组合，大东沟吊大坂铅锌成矿组合) ，洋壳残片成矿组合(大道尔吉铬成矿组合，玉石沟铬成矿组合) ； ( 4 )碰撞造山成矿系统：前陆盆地成矿组合(天鹿铜成矿组合) ，陆内造山韧性剪切成矿组合(寒山鹰咀山金成矿组合) 。
• The ne - trending yiwulushan mountains is located in western liaoning province with the fuxin basin as its western boundary and xialiaohe depression as its eastern boundary . our study area belongs to the fuxin au - concentrating zoning in northeastern part of the yanshan intercontinental orogeny in northern margin of the huabei ( north china ) block , where converge the ew - trending weichang - chifeng - fuxin cu - concentrating zoning in northern yanshan orogeny and the ne - trending suizhong - jinzhou - fuxin au - pb - zn - mo mineralization sequence
  研究区属华北地块北缘的燕山陆内造山带的东北端的阜新金矿集中区，是东西走向的燕山北缘围场-赤峰-阜新金银铜成矿带与北东走向的绥中-锦州-阜新金铅锌钼成矿列的交汇处。

• orogenyとは意味：{名} : 造山運動｛ぞうざん うんどう｝ -------------------------------------------------------------------------------- 【発音】ｏ(:)rα'dзэni、【分節】o?rog?e?ny