秦岭-大别造山带地壳化学结构。
Continental crust chemical structure of Qinling-Dabie Orogen.
造山带地球化学编图的理论探讨。
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.
北淮阳盆岭构造带是大别造山带的重要组成部分。
Beihuaiyang basin and range structural belt is an important part of Dabie orogenic belt.
这为大陆造山带成矿理论的研究提供了新的思维。
Which has provided a new thinking for study of metallogenic theory in the continental orogenic belt.
滇西南造山带的主体由多期变质的岩石单元组成。
The main parts of SW Yunnan orogenic zones consist of complicated metamorphic rock units.
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.
中生界砂岩碎屑组分分析，表明其源区为大别造山带。
Detrital composition analysis of the Mesozoic sandstones indicates that their provenance is the Dabie orogen.
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.
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.
阿尔金构造带包括阿尔金碰撞造山带和阿尔金逆冲-走滑断裂系。
Altyn structural belt consists of collisional orogenic belt and thrusting strike-slip fault systems.
前陆盆地沉积物的岩石学特征反映了双物源供给和造山带的剥蚀。
The lithological feature of the sediments in the foreland basin reflects the double-source supply and the orogenic-belt erosion.
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.
该研究从另一个侧面证明中亚造山带存在一定规模的显生宙陆壳生长。
This study provides new evidence for continental crustal growth in the central Asian orogenic belt during the Phanerozoic.
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?
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 (TanchengLujiang) fault zone.
造山带区域构造演化与大规模成矿作用是同一大陆动力学过程的不同表现。
The regional tectonic evolution and extensive mineralization in orogenic belts are different expressions of the same continental dynamic process.
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.
辽吉古元古宙褶皱带是早前寒武纪时期的一条重要的褶皱造山带与成矿带。
The Liaoji Paleoproterozoic fold zone is an important fold-orogenic and metallogenic zone in the early Precambrian.
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.
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.
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.
该穹隆突出而重要地参与了秦岭造山带的形成与演化，具有重要的大陆动力学意义。
Therefore, it suggests vertical accretion of lithosphere in deep crustal setting of orogenic belts and shows its importance in continental dynamics.
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.
新的资料支持了华北克拉通中部造山带太古宙地质体与其东部陆块存在亲缘关系的认识。
The new data support that idea the Archean geologic body in the Central orogenic belt of the North China craton has affinity with its eastern block.
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