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- Indosinian orogen 印支运动
- 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?
- In printing ink coverage on high indosinian, the multiplicable to overprint. 在油墨覆盖率高的印品上叠印时,可增加保护层。
- Wenquan molybdenum deposit is a porphyry type mineral deposit related with Indosinian granite. 温泉钼矿是与印支期花岗岩有关的斑岩型钼矿床。
- 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。
- Lushan-Pengshan region was a metamorphic core formed by tensional regimes in the early Indosinian orogeny. 庐山-彭山地区原是一个经受印支早期伸展机制下所形成的变质核。
- 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。
- This deposit occurs in Lower Sinian Nantuo sandstone at the exocontact zone of an Indosinian Dashenshan granite stock. 矿床产于印支期大神山花岗岩株外接触带之震旦系下统南沱砂岩组中。
- 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。
- With 300 lines of Photolithography and screen resolution, with cyberctm indosinian. 如果拔取300线网屏的特技拍照制版,不离可得回有动感的印不败品了。
- 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。
- 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 Laozanggou polymetallic ore ares is situated in the central part of the west section of the Indosinian fold system of the southside of Qinling. 老藏沟多金属矿区位于秦岭南侧印支褶皱系西段中部,矿床产于上三叠统陆相火山岩系及其火山构造中。
- 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。
- 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。
- The deposition of the foreland basin and the intracontinental shortening are the response to the Indosinian collision and convergence between the Yangtze and Cathaysian blocks. 这些指示扬子和华夏陆块在印支期发生了强烈陆内碰撞与会聚及前陆盆地的沉积作用。
- Recent studies show, however, that rapakivi granites can be formed in age from Archaean to Phanerozoic and can even occur in orogen. 环斑花岗岩既可以出现于从太古代到显生宙的各个地质时期,也可以产生于造山带中。
- It is a collision suture between the Yangtze Block and North China Block during the Indosinian period, a thrust-napping fault zone belonging to the Tethyan regimes in broad sense. 在印支期由于扬子地块与华北地块的碰撞,成为两板块的对接边界,具有逆冲推覆的性质,属广义的特提斯构造域。
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