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- Qilian Orogen 祁连造山带
- North Qilian orogen belt 北祁连造山带
- North Line:Menyuan and Qilian tour. 北线的门源、祁连风光之旅。
- The Hexi area is located at the tectonic convergence of the North China block and north Qilian Caledonian orogen and Alex block, and is characterized by multiple tectonism that resulted in very rich and complicated geological phenomena. 贺西地区处于北祁连加里东褶皱带、阿拉善地块与鄂尔多斯地块的交汇处,多期构造活动造就了本区复杂的构造和成盆历史。
- South Tianshan: a Late Paleozoic or a Triassic orogen? 南天山:晚古生代还是三叠纪碰撞造山带?
- South Tianshan:a Late Paleozoic or a Triassic orogen? 南天山:晚古生代还是三叠纪碰撞造山带?
- Ore-bearing property of ophiolite in Daban-Dacha area, North Qilian Mts. 北祁连山大坂大岔地区蛇绿岩含矿性。
- Once a snowstorm hit their motor convoy when they were crossing the Qilian Mountains. 有一次当他们车队正在翻越祁连山时，碰到了大风雪。
- The result also support that the Mesoproterozoic orogen in KangdianArea may be related to Grenville orogeny. 富良棚凝灰岩SHRIMP U-Pb年龄也表明康滇南部发育的中元古代晚期造山活动,可能与全球Grenville期造山运动相关。
- The main reason of constitute of shrubbery and its distribution of Qilian Mountain is environmental change. 以气候为主的环境条件变化是祁连山区灌木林的种类组成和分布地域改变的主要原因。
- The Baguashan anticline is located in the western thrust-and-fold zone of Taiwan orogen. 八卦山背斜位于台湾西部的逆冲褶皱带,总体生长是从北向南发展的。
- The middle and lower reaches of the Yangtze River are the foreland tectonic belt of the Dabieshan orogen. 长江中下游地区，是大别造山带的前陆构造带。
- Title： An evaluation of zircon U-Pb dating for metamorphic rocks and comments on zircon ages of Dabie orogen. 关键词：锆石计时;岩浆锆石和变质锆石;蜕晶化作用;增生-混合作用;重结晶作用;大别山年代学
- Geologists at home and aborad are now focusing on research on the Qinling orogen. 秦岭造山带是当今国内外地学界关注的全球性地学研究地区之一。
- A Record of Drought and Flood Series by Tree-Ring Data in the Middle Section of Qilian Mountain Since 904 A.D. 祁连山中部公元904年以来树木年轮记录的旱涝变化。
- The Baguamiao gold deposit is the only superlarge gold deposit in the Qinling orogen. 八卦庙金矿是秦岭造山带唯一的超大型金矿床,曾被认为是微细浸染型(卡林型)金矿。
- The ore-controlling conditions and metallogenic model of Hanshan gold deposit in North Qilian Mts. 甘肃北祁连山寒山金矿床控矿条件与成矿模式。
- Rheology is the liaison between geometry and kinematics as well as dynamics of continental orogen. 流变学研究是大陆造山带几何学、运动学和动力学的桥梁。
- The geological features and genetic pattern of Te-Au deposit related to porphyry in North Qilian Mts. 北祁连山与斑岩有关的碲金型金矿床地质特征和成因模型。
- Hefei Basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu (Tancheng? 合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。
