Disscusion of orogenic geochemical mapping in theory.
造山带地球化学编图的理论探讨。
Beihuaiyang basin and range structural belt is an important part of Dabie orogenic belt.
北淮阳盆岭构造带是大别造山带的重要组成部分。
The main parts of SW Yunnan orogenic zones consist of complicated metamorphic rock units.
滇西南造山带的主体由多期变质的岩石单元组成。
Meanwhile, the fifth stage of magmatism corresponds to the post-orogenic collapse episode.
同时，第五阶段岩浆活动对应于造山后崩塌阶段。
The origins of orogenic belts and basins are two hot topics of current geoscience research.
造山带和盆地成因是当前地学研究的两个热点。
Altyn structural belt consists of collisional orogenic belt and thrusting strike-slip fault systems.
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。
Which has provided a new thinking for study of metallogenic theory in the continental orogenic belt.
这为大陆造山带成矿理论的研究提供了新的思维。
Underfilled peripheral foreland basins develop in the initial stage of intercontinental orogenic belts.
欠补偿周缘前陆盆地发育于陆间造山带的早期阶段。
The dating results provide important data for the evolutionary history of the East Kunlun orogenic belt.
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。
Formation of the basin is closely relative to the development of the South Dabashan-Dahongshan Orogenic Belt.
盆地的形成与南大巴山—大洪山造山带的发育密切相关。
It has been generally considered that orogenic belts and basins are formed by different geodynamic mechanisms.
一般都认为造山带和盆地形成于不同的地球动力学环境。
The Bikou terrane lies at the junction of Qinling orogenic belt, Songpan-Garze orogenic belt and Yangtze Plate.
碧口地块位于秦岭—大别、松潘—甘孜造山带与扬子板块的交汇部位。
The pervasive deformation and internal structure of wide continental orogenic belts indicate non-rigid behavior.
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 Liaoji Paleoproterozoic fold zone is an important fold-orogenic and metallogenic zone in the early Precambrian.
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。
A stable area of continental crust that has not undergone much plate tectonic or orogenic activity for a long period.
大陆地壳长时期内未受到板块构造的或造山活动的很多影响的稳定区。
This study provides new evidence for continental crustal growth in the central Asian orogenic belt during the Phanerozoic.
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。
Two orogenic types, intraplate and marginal orogenies, were recognized by the evidence of main indicators of orogenic process.
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。
The lithological feature of the sediments in the foreland basin reflects the double-source supply and the orogenic-belt erosion.
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。
Because a collision orogenic belt has a complicated crustal structure, new methods have to be adopted for thermal state analysis.
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。
Sedimentary basin and adjacent orogenic belt are two basic tectonic units of continent and twins developed in a geodynamic system.
毗邻的沉积盆地与造山带是大陆构造的基本单元和形成于统一地球动力学系统中的一对孪生体。
The study of volcanic rocks in orogenic belts aims mainly at retracing the tectono_magmatic evolutionary history of orogenic belts.
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。
Dynamic sedimentology of orogenic belts is an important aspect for the research on continental dynamics and geology of orogenic belts.
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。
The coupling relationships between sedimentary basins and orogenic belts refer to all of their interactions in their formation and evolution.
盘山系统形成演化过程中造山带和沉积盆地之间一切相互作用的总和即为盆山间的耦合关系。
The Mujiazhuang copper deposit with high radioactive lead isotope compositions is located in Zha-shan area of the South Qinling Orogenic Belt.
具有高放射性异常铅的穆家庄铜矿床位于南秦岭造山带柞(水)山(阳)地区的泥盆系中。
The regional tectonic evolution and extensive mineralization in orogenic belts are different expressions of the same continental dynamic process.
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 deformation characteristics of Longquanguan DSZ reflect the tectonic evolution of the late Archaean collision orogenic belt in Wutaishan area.
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。
Therefore, it suggests vertical accretion of lithosphere in deep crustal setting of orogenic belts and shows its importance in continental dynamics.
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。
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.
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。
Angular unconformity belongs to an intraplate folded - orogenic deformation. Parallel unconformity is the record of intraplate epeirogenic deformation.
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.
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。
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