1) North Kunlun Orogen
北昆仑造山带
2) Kunlun orogenic belt
昆仑造山带
1.
Discussion on Depositional Characteristics and Basin Quality in Kunlun Orogenic Belt During Early-Middle Devonian;
昆仑造山带早—中泥盆世沉积特征及盆地性质探讨
2.
The results indicate that: in Carboniferous period,Kunlun orogenic belt was in an extension setting,and the north Kunlun was an active margin rift with littoral-neritic sediments of salf-blue water and volcanic basin;the Central Kunlun was an ocean island and underwater uplift,the oceanic islands were denudation areas,whereas the underwater uplifts were mai.
通过多年野外观察、分析测试,结合覆盖全区的1∶250000区域地质调查资料及其他前人研究成果,选择昆仑造山带晚古生代洋盆发育的典型时期石炭纪,对其地层、岩相特征、构造古地理以及构造演化进行了研究。
3.
It was in Paleozoic that the tectonic and deposition system of Kunlun orogenic belt had been formed.
昆仑造山带基本构造-地层格架奠基于古生代,晚泥盆世是加里东造山旋回和华力西造山旋回转换的关键阶段,加里东碰撞造山和其后的伸展裂陷等记录均存在于晚泥盆世沉积地层中。
3) eastern Kunlun orogenic belt
东昆仑造山带
1.
Discovery of Miocene Sporopollen from Matrix Strata of the Naij Tal Group-Complex in the Eastern Kunlun Orogenic Belt;
东昆仑造山带纳赤台岩群基质地层发现中新世孢粉组合
2.
The eastern Kunlun orogenic belt shows characteristics of soft-collision and multi-cycles.
东昆仑造山带具有软碰撞、多旋回的特点 ,造山带内的沉积盆地具有多物源和不同的大地构造背景 。
3.
According to rock characteristics,the Longshigenggongma mélanges(Neoproterozoic Wanbaogou Group—Early Paleozoic Nachitai Group),southern Qingshuiquan,Eastern Kunlun orogenic belt can be divided into 3 types:flysch rock slice,carbonate rock slice and basalt rock slice.
东昆仑造山带清水泉南部的龙什更公玛混杂岩(新元古界万保沟岩群—下古生界纳赤台岩群)按岩性可分为3类岩片:复理石岩片、碳酸盐岩岩片、玄武岩岩片,其中复理石岩片根据其形成年代不同分为新元古界复理石岩片和下古生界复理石岩片。
4) western Kunlun orogenic belt
西昆仑造山带
1.
Magnetic fabric characteristics of main deformation phases in each tectonic unit of the western Kunlun orogenic belt are studied preliminarily in this paper.
文章对西昆仑造山带各构造单元主要变形期的岩石磁性组构特征进行了初步的研究。
5) East Kunlun orogenic belt
东昆仑造山带
1.
Inspirations from the Sino-U.S. cooperative geological mapping in the East Kunlun orogenic belt: ideas and methods
中美合作东昆仑造山带地质填图的启示:填图理念与填图方法
2.
The Wanbaogou Group-complex is a mélange in the East Kunlun orogenic belt,which is composed of two parts:exotic blocks of various ages and matrix strata.
东昆仑造山带万宝沟岩群是一套混杂堆积地层,有外来岩块和基质地层之分,以往根据岩块中的化石将该套地层的时代划为前寒武纪的蓟县纪—青白口纪。
3.
Based on the basin-range coupling theory,the tectonic geology events during Mesozoic and Cenozoic were determined from the point that East Kunlun orogenic belt and west-south Qadam basin were in a common stress field,combining with versatile data and filed geology review.
根据盆山耦合理论,从东昆仑造山带与柴西南盆地受制于共同应力场的角度,结合二者资料及野外考察,对东昆仑山中、新生代以来的构造事件进行了厘定。
6) northern Kunlun collisional orogeny
北昆仑碰撞造山作用
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