2) the Altai Mountains
阿尔泰山南缘
1.
Geology and Geochemistry of the Late Paleozoic Volcanic Rocks of the South Margin of the Altai Mountains and Implications for Tectonic Evolution;
阿尔泰山南缘晚古生代火山岩的地质地球化学特征及其对构造演化的启示
3) Altay orogenic belt
阿尔泰造山带
1.
TIMS U-Pb zircon ages of Fuyun post-orogenic linear granite plutons on the southern margin of Altay orogenic belt and their implications;
阿尔泰造山带南缘富蕴后造山线形花岗岩体锆石U-Pb年龄及其地质意义
2.
The Altay orogenic belt,in Xinjiang,China was formed mainly during late Devonian to early Permian and was mainly a thrust-nappe-detachment orogenesis.
阿尔泰造山带主要形成于晚泥盆世至早二叠世的主造山期,为一冲断-推覆-滑脱的造山作用。
3.
Middle Devonian picrites of the south margin of Altay orogenic belt occur in the lower part of the Beitashan Fm.
阿尔泰造山带南缘中泥盆世苦橄岩位于北塔山组地层的下部,其上依次为玄武岩和安山岩。
4) Altai orogeny
阿尔泰造山带
1.
The Altai orogeny, as one of notable crustal accretion areas, is famous for its abundant mineral deposits.
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。
5) Altaides
阿尔泰造山带
1.
Phase equilibrium of low-pressure metamorphism in the Altaides,Xinjiang;
新疆阿尔泰造山带低压变质作用相平衡研究
2.
After largescale deep-level thrust nappe in Hercynian,the post-orogenic extension occurred in the southern boundary of Altaides,and formed Kelan,Kuerti,Maizi,Areletuobie and Sulubayi metamorphic core complexes.
继大规模海西期深层次逆冲推覆之后,阿尔泰造山带南缘发生了后造山伸展,形成了克兰、库尔提、麦兹、阿热勒托别和苏鲁巴依变质核杂岩。
6) Altay orogen
阿尔泰造山带
1.
The continental collision between Siberian and Kazakhstan-Junggar in Early Carboniferous shaped the large-scale dual thrust-nappe structures in the Altay orogen, NW China.
以上表明,滑动系统、外来系统中的变质岩不属中国阿尔泰造山带的基底岩系,外来系统中的混合花岗岩时代不是海西期,而是加里东期,碰撞期后的隆升剥蚀从南东往北西逐渐减弱。
2.
In the study a systematic finite strain measurement was made on a 50 km-wide section across the Altay orogen in the Fuyun region, with methods such as the dip-isogon of folds, three-dimensional strain of pebbles and S-C angle.
本文采用褶皱等倾线法、砾石三维应变和S-C夹角等应变测量方法,对富蕴地区阿尔泰造山带一个50km的剖面进行了系统的有限应变测算,得出其顺层缩短和剪应变剖面图。
补充资料：泰一
1.亦作"泰壹"。 2.传说中的天神名。 3.中国哲学术语。老子之"道"的别名。有至高﹑唯一之意。
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