| EXAMPLE SENTENCES | ||
|---|---|---|
【大别山超高压变质作用与碰撞造山动力学】，科学出版社。 In "Ultrahigh-pressure metamorphism and collisional dynamics of the Dabie Mountains". eds. | ||
临津江带和沃川带都不具有碰撞造山带的变质特征。 The Imjingang and Ogcheon belts do not exhibit any metamorphic characteristics of collisional orogenic belts. | ||
UHPM记录了显生宙俯冲-碰撞造山带早期碰撞过程中的低热流梯度及陆壳的深俯冲作用。 HPM-UHPM registers the low thermal gradients and deep subduction of continental crust during the early stage of the collision process in Phanerozoic subduction-to-collision orogens. | ||
海拉尔盆地乌尔逊-贝尔凹陷是叠置于内蒙-大兴安岭古生代碰撞造山带的中新生代盆地。 Urxun-Beier depression in Hailaer Basin is the Mesozoic-Cenozoic basin located in the Paleozoic orogenic belt in Inner Mongolia-Daxing'anling area. | ||
该区的碰撞造山作用主要发生在石炭纪和二叠纪，并经历了先挤压后伸展的演化过程。 The collisional orogenesis in the area occurred in the Carboniferous and Permian, and shows the character of the early compression and late extension. | ||
龙泉关韧性剪切带的变形特征反映了五台山晚太古代碰撞造山带的构造演化。 The deformation characteristics of Longquanguan DSZ reflect the tectonic evolution of the late Archaean collision orogenic belt in Wutaishan area. | ||
该蛇绿混杂岩带是义敦碰撞造山带大地构造相中的弧前混杂带相。 The ophiolite melange zone represents forearc melange facies of the Yidun collision orogens. | ||
龙川江盆地是造山带内部发育的新生代小型山间断陷盆地。 Longchuanjiang basin is a small Cenozoic intramontane down-faulted basin. | ||
晓天-磨子潭剪切带的演化指示北大别穹隆是大别造山带晚造山伸展过程中形成的变质核杂岩。 The evolution of the XMSZ demonstrates that the North Dabie dome is a metamorphic core complex developed in the Dabie orogenic belt during post-orogenic extension. | ||
盆地的形成与南大巴山—大洪山造山带的发育密切相关。 Formation of the basin is closely relative to the development of the South Dabashan-Dahongshan Orogenic Belt. | ||
