1.
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
2.
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
3.
Alpine-Himalayan Belt
阿尔卑斯－－喜马拉雅山带
4.
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
5.
Himalayan giant
喜马拉雅山脉中的大山
6.
Darjeeling Himalayan Railway
喜马拉雅山大吉岭铁路
7.
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
8.
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。
9.
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
10.
The Himalayan orogenic belt has some important features that distinguish it from the Andean and Alpine orogenic belts.
喜马拉雅山带不同于安第斯山和阿尔卑斯山，有其自己的特征
11.
The ice on the top of the Himalayas never breaks up
喜马拉雅山山顶的冰从来不化。
12.
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。
13.
Geochemistry and petrogenesis of the Triassic volcanic rocks in the east-central segment of Tethyan Himalaya.
特提斯喜马拉雅带中段东部三叠纪火山岩的地球化学和岩石成因
14.
Volcanic Rocks in the Central Belt of Tethyan Himalayas Since the Late Paleozoic and Their Implications;
特提斯喜马拉雅带中段晚古生代以来的火山岩及其意义
15.
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
16.
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
17.
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
18.
Attribution of the Qinghai-Tibet Plate and Himalayan Orogeny
青藏板块属南大陆范畴及喜马拉雅现代造山运动