Cite
Source amplitudes of volcano-seismic signals determined by the amplitude source location method as a quantitative measure of event size
MLA
Yuta Maeda, et al. “Source Amplitudes of Volcano-Seismic Signals Determined by the Amplitude Source Location Method as a Quantitative Measure of Event Size.” Journal of Volcanology and Geothermal Research, vol. 257, May 2013, pp. 57–71. EBSCOhost, widgets.ebscohost.com/prod/customlink/proxify/proxify.php?count=1&encode=0&proxy=&find_1=&replace_1=&target=https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&scope=site&db=edsair&AN=edsair.doi...........6245e86dbcb2e41e9ed83b10b67c9801&authtype=sso&custid=ns315887.
APA
Yuta Maeda, Hiroyuki Kumagai, Rudy Lacson, Tadashi Yamashina, Mario Ruiz, Hugo Yepes, Melquiades S. Figueroa, P. Palacios, & H. D. Ortiz. (2013). Source amplitudes of volcano-seismic signals determined by the amplitude source location method as a quantitative measure of event size. Journal of Volcanology and Geothermal Research, 257, 57–71.
Chicago
Yuta Maeda, Hiroyuki Kumagai, Rudy Lacson, Tadashi Yamashina, Mario Ruiz, Hugo Yepes, Melquiades S. Figueroa, P. Palacios, and H. D. Ortiz. 2013. “Source Amplitudes of Volcano-Seismic Signals Determined by the Amplitude Source Location Method as a Quantitative Measure of Event Size.” Journal of Volcanology and Geothermal Research 257 (May): 57–71. http://widgets.ebscohost.com/prod/customlink/proxify/proxify.php?count=1&encode=0&proxy=&find_1=&replace_1=&target=https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&scope=site&db=edsair&AN=edsair.doi...........6245e86dbcb2e41e9ed83b10b67c9801&authtype=sso&custid=ns315887.