在造山的过程中，一些非常古老的沉积物已被转化为火成岩和变质岩，已经无法辨认了。
Some very ancient sediments were no longer recognizable, having been converted to igneous and metamorphic rocks in the course of mountain building.
造山带地球化学编图的理论探讨。
秦岭-大别造山带地壳化学结构。
Continental crust chemical structure of Qinling-Dabie Orogen.
楔入构造活动是秦岭造山带的成山模型。
So Wedging was the mechanism for mountain building in the Qinling orogen.
造山带和盆地成因是当前地学研究的两个热点。
The origins of orogenic belts and basins are two hot topics of current geoscience research.
碰撞造山作用是一个在碰撞事件之后的均变过程。
The collision orogeny is a uniformitive process after the collision event.
欠补偿周缘前陆盆地发育于陆间造山带的早期阶段。
Underfilled peripheral foreland basins develop in the initial stage of intercontinental orogenic belts.
人工造山在中国传统造园中便自然占有十分突出的地位。
Artificial orogeny in traditional Chinese garden occupies a very prominent position and natural.
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.
南海北部陆缘在中生代晚期曾形成宏伟的华夏陆缘造山带。
There was an orogenic belt called the Cathaysian continental marginal orogenic belt in late Mesozoic along the present northern margin of the South China Sea.
大量透入性变形和巨型大陆造山带内部构造显示非刚性特征。
The pervasive deformation and internal structure of wide continental orogenic belts indicate non-rigid behavior.
一种可导致形成造山带和俯冲带的岩石圈板块间的相互作用。
An interaction of lithospheric plates that can result in the formation of mountain belts and subduction zones.
所以，用鼹鼠丘造山，其实就是把小事说成大事，言过其实了。
So - making a mountain out of a molehill means making a small problem seem like a big one.
造山带动力沉积学是造山带地质学和大陆动力学研究的重要方面。
Dynamic sedimentology of orogenic belts is an important aspect for the research on continental dynamics and geology of orogenic belts.
测年结果为研究东昆仑造山带的演化历史提供了重要的年代学资料。
The dating results provide important data for the evolutionary history of the East Kunlun orogenic belt.
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。
Plate tectonic analysis of basin systems interspersed in orogenic belts requires that the effects of approximation be carefully distinguished from those of separation.
它们的形成构造环境由陆缘碰撞造山环境向造山晚期或造山后环境演化。
The tectonic environment of forming these units develops the epicontinental-collison orogenic environment to the late-orogenic or post-orogenic environment.
这些证据为华南的三叠纪造山作用和构造演化模式提供了强有力的支持。
These evidences provide forceful support for tectonic interpretation of the Triassic orogeny and the tectonic evolution model in South China.
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu Tancheng?
角度不整合是板内褶皱造山变形，平行不整合是板内造陆变形的重要记录。
Angular unconformity belongs to an intraplate folded - orogenic deformation. Parallel unconformity is the record of intraplate epeirogenic deformation.
造山带火山岩石学研究的主要目的在于重溯造山带的构造-岩浆演化历史。
The study of volcanic rocks in orogenic belts aims mainly at retracing the tectono_magmatic evolutionary history of orogenic belts.
根据造山作用的主要标志识别出板内造山和板缘造山两种主要造山作用类型。
Two orogenic types, intraplate and marginal orogenies, were recognized by the evidence of main indicators of orogenic process.
在造山活动中，火山口中心地带提升，产生了一个直径约7公里的小型火山口。
During an impact event that creates a crater, central uplifts or mounds form on the floor of the crater in craters larger than 7km in diameter.
位于大别造山带北部的合肥盆地，其中的沉积是造山带剥露历史的重要记录。
Sediments in the Hefei basin to the north of the Dabie orogen are important records of unroofing history for the orogen.
具“S”型花岗岩的特征，互相呈脉动侵入接触关系，形成于板内同造山期的环境。
It has features of "s" granite and as pulsation intrusion contact and formed the intraplate synorogenic period setting.
由于碰撞造山带具有的地壳结构的复杂性，必须采用新的研究方法来分析其热结构。
Because a collision orogenic belt has a complicated crustal structure, new methods have to be adopted for thermal state analysis.
多岛弧造山模式和多机制的隆升模式等大陆动力学问题也是层序地层所遇到的新挑战。
Sequence stratigraphy will be encountered with new challenges from continental dynamics of archipelago arc orogenic models and multi mechanism uplifting models.
阿尔泰造山带是中亚地区显生宙大陆地壳增生明显的地区之一，蕴藏丰富的矿产资源。
The Altai orogeny, as one of notable crustal accretion areas, is famous for its abundant mineral deposits.
阿尔泰造山带是中亚地区显生宙大陆地壳增生明显的地区之一，蕴藏丰富的矿产资源。
The Altai orogeny, as one of notable crustal accretion areas, is famous for its abundant mineral deposits.
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