Intracontinental相关论文
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Ore fluid of the Tieluping silver deposit of Henan Province and its illustration of the tectonic mod
The Tieluping silver deposit, located in the NE-trending faults within the metamorphic basement of the Xiong’er Mountai......
The Yanshan movement/orogeny has been proposed for 90 years, which is of special significance in the history of geologic......
Application of grouped detrital zircon analyses to determine provenance and closely approximate true
In the Lower Cretaceous McMurray-Clearwater succession of the intracontinental Alberta Foreland Basin, Canada, detrital ......
Application of grouped detrital zircon analyses to determine provenance and closely approximate true
In the Lower CretaceousMcMurray-Clearwater succession of the intracontinental Alberta Foreland Basin,Canada,detrital zir......
在对龙门山的构造变形、沉积环境、地层古生物、石油地质、遥感地质、地球物理、同位素地质等专题研究基础上,综合归纳出龙门山造......
Multistage Enrichment of the Sawafuqi Uranium Deposit： New Insights into Sandstone-hosted Uranium De
在 Tian 掸人 orogenic 带的中央新生代 intracontinental orogenic 过程在 intramontane 盆和邻近 orogen 的那些在招待沙岩的铀......
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Mineralization during Collisional Orogenesis and Its Control of the Distribution of Gold and Other D
The Junggar orogen, Xinjiang, China, is an important part of the Ural-Mongolian orogen.The collisional orogenesis in thi......
The Huanan (South China) subcontinent was created by amalgamation of the Yangtze, Xianggan, Ca-thaysia and Zhemin microc......
The post-Mesoproterozoic tectonometamorphic history of the Musgrave Province,central Australia,has previously been solel......
Tectonically the Dabie orogenic belt consists mainly of the Dabieshan Yanshanian uplifted zone and the Beihuaiyang Varis......
准噶尔造山带是乌拉尔—蒙古造山带的重要组成部分。该区的碰撞造山作用主要发生在石炭纪和二叠纪,并经历了先挤压后伸展的演化过......
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Rhyacian and Neoproterozoic magmatic associations of the Gurupi Belt,Brazil: Implications for the te
The Gurupi Belt,in north-northeastern Brazil,is a mobile belt developed in the south-southwestern margin of the Sao Luis......
Based on the discussion on the intracontinental orogenic igneous rocks formed after India- Asia collision (40 or 45 Ma )......
