stands for Digital Object Identifier
and is the unique identifier for objects on the internet. It can be used to create persistent link and to cite articles.
Using DOI as a persistent link
To create a persistent link, add「http://dx.doi.org/」
before a DOI.
For instance, if the DOI of an article is 10.5297/ser.1201.002 , you can link persistently to the article by entering the following link in your browser: http://dx.doi.org/ 10.5297/ser.1201.002 。
The DOI link will always direct you to the most updated article page no matter how the publisher changes the document's position, avoiding errors when engaging in important research.
Cite a document with DOI
When citing references, you should also cite the DOI if the article has one. If your citation guideline does not include DOIs, you may cite the DOI link.
DOIs allow accurate citations, improve academic contents connections, and allow users to gain better experience across different platforms. Currently, there are more than 70 million DOIs registered for academic contents. If you want to understand more about DOI, please visit airiti DOI Registration （ doi.airiti.com ） 。
楊曉明 , Masters Advisor：鍾孫霖
繁體中文 DOI： 10.6342/NTU.2008.02870
- Barley, M. E., Pickard, A.L., Khin, Zaw, Rak, P. and Doyle, M.G., 2003, Jurassic to Miocene magmatism and metamorphism in the Mogok metamorphic belt and the India-Eurasia collision in Myanmar. Tectonics, doi: 10.1029/ 2002TC001398.
- Bertrand, G., Rangin, C., Maluski, H., Han, T.A., Thein, M., Myint, O., Maw, W. and Lwin, S., 1999, Cenozoic metamorphism along the Shan scarp (Myanmar): Evidence for ductile shear along the Sagaing fault or northward migration of the eastern Himalayan syntaxis?. Geophysical research letters, 26, 915-918.
- Bertrand, G., Rangin, C., Maluski, H., Bellon, H. and the GIAC Scientific Party, 2001, Diachronous cooling along the Mogok metamorphic belt(Shan scarp, Myanmar): The trace of the northward migration of the Indian syntaxis. Journal of Asian Earth Sciences, 19, 649-659.
- Bertrand, G. and Rangin, C., 2003, Tectonics of the western margin of the Shan plateau (central Myanmar): implication for the India-Indochina oblique convergence since the Oligocene. Journal of Asian Earth Sciences, 21, 1139-1157.
- Chung, S.L., Chu, M.F., Zhang, Y., Xie, Y., Lo, C.H., Lee, T.Y., Lan, C.Y., Li, X., Zhang, Q. and Wang, Y., 2005, Tibetan tectonic evolution inferred from spatial and temporal variations in post-collisional magmatism. Earth- Science Reviews, 68, 173-196.
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