Gempa bumi Bali 1917: Perbedaan antara revisi

Pulau Bali merupakan bagian dari [[Busur Sunda]], yang terbentuk di atas [[batas konvergen]] di mana Lempeng Australia yang [[subduksi]] di bawah [[Lempeng Sunda]]. Laju konvergensi di [[Palung Sunda|Parit Sunda–Jawa]] adalah 7,5 &nbsp;cm per tahun.<ref name="McCaffrey">{{cite journal|last=McCaffrey|first=R.|year=1987|title=Earthquakes, gravity, and the origin of the Bali Basin: an example of a nascent continental fold-and-thrust belt|url=http://web.pdx.edu/~pdx07343/www/pubs/mccaffrey_bali_jgr_1987.pdf|journal=Journal of Geophysical Research|publisher=[[National Academy of Sciences]]|volume=92|issue=B1|pages=441–460|doi=10.1029/jb092ib01p00441|author2=Nabelek J.|accessdate=10 November 2012|archive-date=2013-12-11|archive-url=https://web.archive.org/web/20131211185118/http://web.pdx.edu/~pdx07343/www/pubs/mccaffrey_bali_jgr_1987.pdf|dead-url=yes}}</ref>