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 ） 。
- Bowen, N. L. (1922) The reaction principle in petrogenesis. Journal of Geology, 30, 177-198.
- Bultitude, R. J., and Green, D. H. (1971) Experimental study of crystal-liquid relationships at high pressures in olivine nephelinite and basanite compositions. Journal of Petrology, 12, 121-147.
- Chen, C. H., Chung, S. L., and Lee, C. Y. (1987) Genesis of Neogene continental margin alkali basalts and tholeiites in Western Taiwan and the significance of high-pressure megacrysts and lherzite inclusion. Acta Geol. Taiwanica, 25, 111-132.
- Chung, S. L., Sun, S. S., Tu, K., Chen, C. H., and Lee, C. Y. (1994) Late Cenozoic basaltic volcanism around the Taiwan Strait, SE China: product of lithosphere-asthenosphere interaction during continental extension. Chemical Geology, 112, 1-20.
- Chung, S. L., Jahn, B. M., Chen, S. J., Lee, T., and Chen, C. H. (1995a) Miocene basalts in northwestern Taiwan: evidence for EM-type mantle sources in the continental lithosphere. Geochimica et Cosmochimica Acta, 59, 3, 549-555.
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