1.
HIMALAYAN COLLISION OROGENESIS AND FORMATION OF THE LARGE ENRICHED MINERAL DISTRICT: SCIENTIFIC PROBLEMS AND THINKING
喜马拉雅碰撞造山作用与(超)大型矿集区的形成:科学问题与思考
2.
The frequency dispersions of Rayleigh waves and 3-D velocity structures in Himalayan collision orogenic zone and Qiangtang basin
喜马拉雅碰撞造山带和羌塘盆地的瑞雷波频散与三维速度结构
3.
Intracontinent Orogen and Metallogenesis in Himalayan Epoch:Changdu Large Composite Basin, Eastern Tibet
藏东缘昌都大型复合盆地喜马拉雅期陆内造山与成矿作用
4.
The Indian subcontinent detaching itself from Antarctica and sweeping across the Indian Ocean to its violent collision with Asia's landmass across the Himalayas;
印度次大陆从南极洲脱离，漂过印度洋越过喜马拉雅山与亚洲陆块猛烈碰撞；
5.
The present thickenning of Northern Qilian orogenic belt is the result of himalayan reorogency.
而现今的北祁连造山带的缩短和抬升则为喜马拉雅期再造山作用的产物
6.
Himalayan giant
喜马拉雅山脉中的大山
7.
Alpine-Himalayan Belt
阿尔卑斯－－喜马拉雅山带
8.
Darjeeling Himalayan Railway
喜马拉雅山大吉岭铁路
9.
In South Asia, the Himalayan glaciers could retreat causing water scarcity.
在南亚，喜马拉雅山冰河的倒退造成了水荒。
10.
Stratiform Geomorphology and Himalayan Tectonic Movement on the North China Mountains;
中国华北山地的层状地貌与喜马拉雅构造运动
11.
METAMORPHISM EVOLUTION OF THE LATE ARCHEAN COLLISION OROGENIC BELT IN WUTAISHAN
五台山晚太古代碰撞造山带的变质作用演化
12.
The end of the sedimentation of the foreland basin indicates completion of the collisional orogeny.
前陆盆地的终结标志着碰撞造山作用的结束。
13.
Early Paleozoic Collisional Orogeny and Magmatism on Northern Margin of the Qaidam Basin
柴达木盆地北缘早古生代碰撞造山及岩浆作用
14.
DISCOVERY OF COESITE-BEARING ECLOGITE FROM WEST HIMALAYAN TECTONIC LINK AND ITS ENLIGHTENMENT
喜马拉雅造山带西构造结含柯石英榴辉岩的发现及其启示
15.
Evolution of Deformation and Metamorphism During the Tectono Emplacement of the Granulite in the Middle Himalaya Orogen
喜马拉雅造山带中段麻粒岩构造侵位过程中变质变形演化
16.
The ice on the top of the Himalayas never breaks up
喜马拉雅山山顶的冰从来不化。
17.
Truth is, the Himalayas are between you two, and China's never coming over the Himalayas.
事实是：喜马拉雅山就在你们中间，而中国是从不翻越喜马拉雅山的。
18.
INFERRING THE TECTONIC STRESS FIELD OF HIMALAYA ARCUATE STRUCTURE FROM THE MULTIPLE FOCAL MECHANISMS
由多个地震的震源机制解推断喜马拉雅弧形山系的构造应力场