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 ） 。
- Allen, C.R., Gillespie, A.R., Yuan, H., Sieh, K.E., Buchun, Z., and Chengnan, Z., 1984, Red River and associated faults, Yunnan Province, China: Quaternary geology, slip rates, and seismic hazard Geological Society of America Bulletin. , v. 95, p. 686-700.
- Bell, T.H., and Forde, A., 1995, On the significance of foliation patterns preserved around folds by mineral overgrowth: Tectonophysics, v. 246, p. 171-181.
- Bell, T.H., Ford, A., and Wang, J., 1995, A new indicator of movement direction during orogenesis: measurement technique and application to the Alps: Terra Nova, v. 7, p. 500-508.
- Bell, T.H., and Hickey, K.A., 1997, Distribution of pre-folding linear indicators of movement direction around the Spring Hill Synform, Vermont significance for mechanism of folding in this portion of the Appalachians: Tectonophysics, v. 274, p. 275-294.
- Bell, T.H., and Hickey, K.A., 1998, Multiple deformations with successive subvertical and subhorizontal axial planes in the Mount Isa region their impact on geometric development and significance for mineralization and exploration: Economic Geology, v. 93, p. 1369-1389.
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