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 ） 。
吳詩敏 , Masters Advisor：李通藝;葉孟宛
- Attoh, K., Dallmeyer, R.D., and Affaton, P., 1997, Chronology of nappe assembly in the Pan-African Dahomeyide orogen, West Africa: evidence from 40Ar39Ar mineral ages: Precambrian Research, v. 82, p. 153-171.
- Bertrand, J.M., and Jardim de Sà, E.F., 1990, Where are the Eburnean-Transamazonian collisional belts?: Canadian Journal of Earth Sciences, v. 27, p. 1382-1393.
- Bessoles, B., and Trompette, R., 1980, Géologie de l'Afrique. La chaîne panafricaine: "zone mobile d'Afrique Centrale (partie sud) et zone mobile soudanaise": Mémoire du B.R.G.M., France, v. 92, p. 396.
- Binks, R.M., and Fairhead, J.D., 1992, A plate tectonic setting for Mesozoic rifts of West and Central Africa: Tectonophysics, v. 213, p. 141-151.
- Castaing, C., Feybesse, J.L., Thiéblemont, D., Triboulet, C., and Chèvremont, P., 1994, Palaeogeographical reconstructions of the Pan-African/Brasiliano orogen: closure of an oceanic domain or intracontinental convergence between major blocks?: Precambrian Research, v. 69, p. 327-344.
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