1) the Orogenic-Sedimentology
造山带沉积学
1.
Through study of the sedimentaiy geology in the several main belts in China, it is mainly purpose that paper introduces the classic sedimentology to a research on the formation and evolution of erogenic belts and builds up a relatively systemic method and theory of the Orogenic-Sedimentology.
论文通过对中国西南及邻区主要造山带的沉积地质学研究，将经典的沉积学方法体系引入造山带的形成和演化研究，建立了一个比较完整的造山带沉积学理论和方法体系。
2) basin analysis of orogenic belt
造山带沉积盆地分析
3) structural-depositional belt
构造沉积带
4) tectonic-sedimentology
构造沉积学
1.
This paper studies systematically the evolution features of south fault of Zhu Ⅲ Depression in plane and vertical direction and its control over sedimentary system types and their distribution during the fault-rifted lake period according to the fundamental concept of tectonic-sedimentology and the analysis of paleo-subsiding rate and paleo-tectonic deformation rate recovered by back-stripping.
运用构造沉积学基本概念,在使用回剥法恢复古沉降速率和古构造活动速率法的基础上,系统地分析了珠江口盆地珠三坳陷南部控坳断裂在断陷湖盆期的平面和垂向演化特征及其对沉积体系类型与展布的控制作用。
5) volcano-sedimentary assemblages
火山-沉积建造
6) post-orogenic deposit
造山后沉积极
补充资料：阿尔卑斯造山带
欧洲的阿尔卑斯以及其它一些年青的巨大造山带和褶皱山系。早第三纪和晚第三纪由于阿尔卑斯运动(中国称喜马拉雅运动)，使沿欧洲南部中生代的古地中海发生了强烈褶皱，形成横贯东西的阿尔卑斯-喜马拉雅山脉(从西班牙至亚洲南部)。严格地说，此词只限于造山带的北翼，由徐士(E.Suess)创名。同义词有“地中海带”、“阿尔卑斯-喜马拉雅带”。板块构造学说认为，这个造山带属碰撞型山链。(共213字)
【引用信息】徐世芳，李博主编.地震学辞典.北京：地震出版社.2000.第5页.
【引用信息】徐世芳，李博主编.地震学辞典.北京：地震出版社.2000.第5页.
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