1) tectonic zone of Middle Asia
中亚构造带
2) Central Asian Orogenic Belt
中亚造山带
1.
Paleozoic-Mesozoic granites in the Central Asian orogenic belt have commonly positiveεNd values, implying large-scale continental crustal growth in the Phanerozoic.
本文从中亚造山带显生宙花岗岩同劳亚大陆的关系出发,进一步探讨超大陆演化、大陆地壳生长和地幔中俯冲板片雪崩事件(slab avalanche events)三者之间的关系,强调在超大陆形成时伴随大陆地壳急剧生长,在超大陆裂解、离散时大陆地壳的生长和消亡大体上保持平衡。
3) CAOB
中亚造山带
1.
It is well known that the Central Asian Orogenic Belt (CAOB) is the largest and most typical accretionary orogenic belt in the world.
中亚造山带是世界上最大的增生型造山带之一。
4) central structural zone
中央构造带
1.
On the basis of regional geologic background, the analyses on core, grain size, thin section, shape of the log curves show that the western part of the central structural zone of Dongying sag mainly belongs to turbidity facies in the early and middle period of the middle section in the third member of Shahejie Formation.
从区域地质背景出发 ,对岩心观察、粒度分析、镜下鉴定结果及测井曲线形态等进行的综合分析表明 ,东营凹陷中央构造带西段Es中3沉积早中期主要属于半深湖—深湖背景下的浊积扇相沉积 ,Es中3沉积中后期属浊积扇相和三角洲相沉积。
5) middle structural belt
中部构造带
6) the central tectonic zone
中轴构造带
1.
From systematic analysis and synthesis of geological surveying and geophysical exploring data, it is known that the central tectonic zone on the mainland of China is characterized by segmentation of active tectonics and various active crustal shortening structures.
文中通过对已有地质调查和地球物理探测成果的系统分析与综合 ,给出了中轴构造带地表活动构造的分段特征 ,特别是近地表显示地壳缩短变形的挤压构造特征 ;初步论证了中轴构造带中南段为岩石圈深度范围阻挡青藏高原物质东向或南东向滑移的阻挡构造边界 ,且具有上、下呼应的深浅构造关系 ;指出中轴构造带内部活动挤压构造具有把青藏高原北西向左旋走滑控制的块体东向或南东向滑移转换成为隆升运动的构造转换作用 ;对其中南段整体的综合研究有助于深刻理解中国大陆最新构造变动和地震时空迁移的动力学问题。
补充资料：板带轧制速度规程(见板带轧制规程设计)
板带轧制速度规程(见板带轧制规程设计)
speed schedule for plate and strip rolling
bandai zhazhi sudu guieheng板带轧制速度规程(speed seheduxe fo:plateand strip rolling)见板带札制规程设计。
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