板内造山带,intraplate orogenic belt
1)intraplate orogenic belt板内造山带
1.The main characteristic ofintraplate orogenic belts is its re mobilization of the stable lithosphere consolidated in the earlier stage There are two fundamental features ofintraplate orogenic belts, i.板内造山带的基本特征是前期已经固结的岩石圈重新活化。
2.The different opinions concerning the concept ofintraplate orogenic belt are firstly reviewed in this paper.讨论了关于板内造山带含义的不同认识。
3.The northern Qilian orogenic belt is anintraplate orogenic belt formed on the basis of the Neoproterozoic craton.北祁连山是发育在新元古代大陆克拉通背景上的板内造山带，它的形成经历了三个构造发展阶段：（１） 早古生代是克拉通裂解的拗拉槽而不是大洋盆地，其西延部受阿尔金断裂左行错移约３５０ ～４００ ｋｍ ，对应于塔里木盆地北部的满加尔 阿瓦提坳陷，它们共同构成了“西域板块”之上的震旦纪 早古生代统一的拗拉槽，早古生代末“祁连事件”使拗拉槽闭合形成古祁连山。
英文短句/例句
1.Tectonic evolutionary characteristics of Yanshanian intraplate orogenic belt in Mesozoic era燕山板内造山带中生代构造演化特征
2.The Mesozoic Structural Framework and Evolution in the Eastern Segment of the Yanshan Intraplate Orogen;燕山板内造山带东段中生代构造格局及形成演化
3.Clenched in the volcanic fist, the huge Basin was created By the motion of crustal plates.这个巨大的盆地坐落在火山带内，它是由地壳板块的运动所造成的。
4.Characters of Later Jurassic Yinshan Intraplate Orogeny Belt--Evidence from Daqing Shan,Inner Mongolia阴山晚中生代板内造山特征及其动力机制——以内蒙古大青山为例
5.<title>DISCUSSION ON PLATE TECTONICS AND?MINERALIZING PROCESS IN MIDDLE?LATE?PROTEROZOIC EON IN QINLING OROGENIC BELT?AND ITS ADJACENT AREA秦岭造山带及邻区中晚元古宙板块构造与成矿作用初析
6.Intraplate Tectonics of Bogda Mountain in Xingjiang and Its Adjacent Plates;新疆博格达山及其邻区板内构造作用研究
7.POSITIVE DECOLLEMENT AND MINERALIZATION OF INTRAPLATE CALEDONIAN POSTORGENIC PHASE ON THE BORDER OF HUNAN AND GUIZHOU PROVINCES湘黔边境加里东板内造山期后正向滑脱构造与成矿
8.Timing of the Transformation from Seafloor Spreading on the South Margin of the North China Block to Subduction within the North Qinling Orogenic Belt从华北陆块南缘大洋扩张到北秦岭造山带板块俯冲的转换时限
9.Impact of Sliding Structure on Ⅱ 1 Coal Roof Engineering Geological Zonality in Songshan Minefield嵩山井田滑动构造对二_1煤层顶板岩体分带性的影响
10.Research on Metallogenic Series and Prognosis of Endogenetic Metallic Deposits in the Middle Section of Tianshan-Xingmeng Orogen;天山—兴蒙造山带中段内生金属矿床成矿系列及成矿预测
11.The rocks coexist closely, distributing in a narrow and long belt in the Late Precambrian orogenic belt in northern Liaoning.它们紧密共生，呈狭长的带状分布于辽宁北部晚前寒武纪造山带内。
12.IDENTIFICATION AND IMPLICATION OF THE ORINGINAL NNE-TRENDING STRUCTURE OF QINLING GROUP IN THE QINLING OROGENIC BELT秦岭造山带中秦岭群内初始北北东向构造方位及其地质意义
13.The west Tianshan rich Fe ore belt, Xinjiang autonomous region lies in the introvolcanic arch basin at the east end of Yili plate.新疆西天山富铁矿成矿带位于伊犁板块东端,火山岛弧带弧间断陷盆内。
14.Plate Tectonics and Geodynamics of Orogenesis of the Southwest Tianshan Mountains;西南天山板块构造及造山运动动力学
15.Mesozoic deformation of Dabashan curvilinear structural belt of Qinling orogen秦岭造山带大巴山弧形构造带中生代构造变形
16.Plate tectonic analysis of basin systems interspersed in orogenic belts requires that the effects of approximation be carefully distinguished from those of separation.分析造山带中盆地系的板块构造时，需要将靠近作用与分离作用仔细区分开来。
17.TECTONIC EVOLUTION OF THE LATE ARCHEAN WUTAISHAN COLLISION OROGEN五台山晚太古代碰撞造山带构造演化
18.Large-Scale Metallogeny in the Continental Evolution: Examples of Three Typical Orogenic Belts in China;中国若干典型陆内造山带演化过程与大规模成矿作用初探
相关短句/例句
Yanshan Intraplate orogen燕山板内造山带
1.On Yanshan intraplate orogene: An example from Taiyanggouarea, Lingyuan, western Liaoning Province, Northeast China;燕山板内造山带早期构造变形演化——以辽西凌源太阳沟地区为例
3)Yanshan intraplate orogenic belt燕山板内造山带
4)intraplate orogeny板内造山
1.Late Cenozoicintraplate orogeny and dynamic metallogeny in the southern Qinghai-Tibet Plateau;青藏高原南部晚新生代板内造山与动力成矿
2.Characters of Later Jurassic Yinshan Intraplate Orogeny Belt——Evidence from Daqing Shan,Inner Mongolia阴山晚中生代板内造山特征及其动力机制——以内蒙古大青山为例
3.Involved in the Cenozoicintraplate orogeny of southwestern Tianshan,the northwestern Tarim Basin had developed a series of NE-trending faults and fault-related folds.塔里木盆地西北部卷入了西南天山新生代板内造山活动,以发育一系列北东向展布的断层和断层相关褶皱为特征,但该区新生代构造变形的原因尚存在争议。
5)plate marginal orogenic belt板缘造山带
1.It is stressed that the intraplate orogenic belt is a distinct new type of orogen rather than a successor of an interplate orplate marginal orogenic belt.指出板内造山带是一种特殊类型的造山带，而不是板缘造山带或板间造山带持续发展的结果。
6)interior orogen内部造山带
1.This orogen saw a very complicated history frominterior orogen to peripheral orogen and tointerior orogen again.该造山带经历了边缘造山带-内部造山带-边缘造山带相继转化的过程,它控制了加里曼丹的区域成矿作用,特别是晚渐新世-中中新世北加里曼丹内部造山带的逆冲叠瓦阶段是加里曼丹区域成矿的最重要时期。
延伸阅读
板带轧制速度规程(见板带轧制规程设计)板带轧制速度规程(见板带轧制规程设计)speed schedule for plate and strip rollingbandai zhazhi sudu guieheng板带轧制速度规程(speed seheduxe fo:plateand strip rolling)见板带札制规程设计。
