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1)  Altun orogenic belt
阿尔金造山带
1.
The inversion for the Q value of the upper crust along the profile from Baicheng to Da Qaidam has been carried out using seismic reflection/refraction data acquired on the profiles which cross the Tarim basin, the Altun orogenic belt and the Qaidam basin, respectively.
利用横跨塔里木盆地、阿尔金造山带和柴达木盆地的拜城—大柴旦综合地球物理剖面的人工地震宽角反射 折射资料 ,对拜城—大柴旦剖面研究区上地壳的Q值结构进行了反演 。
2)  Eastern Altun orogenic belt
阿尔金造山带东段
3)  Altyn collisional orogenic belt
阿尔金碰撞造山带
1.
The displacement of Altyn nappe-strike slip fault system since the Meozoic modifies the former Altyn collisional orogenic belt,which resulted in the formation of a series of Jurassic sedimentary basins within the Altyn Mountain and the southeastern part of the Tarim basin.
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。
4)  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。
5)  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。
6)  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。
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.
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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