1) Laji orogenic belt
拉脊山造山带
1.
The Laji orogenic belt has a basement of Jinning epoch.
拉脊山造山带是在晋宁期基底上 ,由于断裂作用而形成的。
2) Lajishan fault
拉脊山断裂带
1.
Lajishan fault appears obvious linear tectonic characteristics in remote sensing photos,which is formed by the northern and southern marginal Lajishan faults in NE direction,and it is the boundary zone of Xining-Minhe basin in the north,Xunhua-Hualong basin in the south,Linxia basin in the east and other Late Neozoic era downfaulted basins.
拉脊山断裂带在遥感影像上具有明显的线性构造特征,由拉脊山北缘断裂带和拉脊山南缘断裂带向北东凸出的弧形挤压逆冲断裂带构成,成为北侧的西宁—民和盆地、南侧的循化—化隆盆地和东侧的临夏盆地等多个晚新生代断陷盆地的边界,拉脊山北缘断裂带全长230km,由数段弧状不连续的断裂带组成。
3) Lajishan
拉脊山
1.
Characteristics and Tectonic Affinity of Lajishan Paleo-Mantle in Qilian Orogenic Belt: A Geochemical Study of Basalts;
祁连造山带中部拉脊山古地幔特征及其归属:来自基性火山岩的地球化学证据
2.
Metamorphic Core Complex Structure and Uplifting Mechanism in Lajishan-Hualong Area;
拉脊山-化隆变质核杂岩构造及其隆升机制探讨
3.
Entering Construction Scheme of Lajishan Tunnel Exit;
拉脊山隧道出口进洞施工方案
4) Atlas orogenic zone
阿特拉斯造山带
5) Kelamaili orogenic belt
克拉麦里造山带
1.
Located on the northeastern margin of Junggar basin,the Kelamaili orogenic belt was an important tectonic unit in central Asia geology.
据此推论克拉麦里洋盆封闭于早石炭世晚期,克拉麦里造山带在侏罗纪早期发生快速隆升。
2.
The Kelamaili orogenic belt, located on the northeastern margin of the Junggar basin, is an important tectonic unit in the Central Asian tectonic framework.
克拉麦里造山带位于准噶尔盆地东北缘,是中亚构造框架中一个非常重要的构造单元,研究工作较多,但对其演化历史一直存在不同认识。
6) Himalayan orogen
喜马拉雅造山带
1.
Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry,exhumation history,and foreland sedimentation;
喜马拉雅造山带新生代构造演化:沿走向变化的构造几何形态、剥露历史和前陆沉积的约束
2.
The uplift of the Himalayan orogen is an interesting geological problem.
喜马拉雅造山带的隆升,在地质学研究中是一个非常让人感兴趣的问题,为了对其进行定量研究,揭示隆升历史及幅 度等相关问题,运用磷灰石、锆石裂变径迹法对研究区淡色花岗岩进行了分析,所取样品的裂变径迹年龄位于17。
3.
The study area lying in the north slope of the middle part of Himalayan orogen involves abundant representative tectonic landforms.
研究区位于喜马拉雅造山带中段北坡,构造地貌丰富、典型。
补充资料：弗格拉什山
弗格拉什山
罗马尼亚南喀尔巴阡山脉的最高山块。在奥尔特河与登博维察河上源之间。长约50公里。主要由结晶岩组成。山势雄伟高峻，北陡南缓。北坡山脊耸立着多座2，000米以上的锯齿形山峰，最高峰摩尔多韦亚努峰，海拔2，543米。有冰斗和冰碛湖等。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条