Arcus insularum

Arcus insularum est longa montium igniferorum actuosorum catena ubi terraemotus saepe fiunt, secundum convergentes laminarum tectonicarum fines, sicut Circulum Ignis in Oceano Pacifico. Plurimi arcus insularum ex crusta oceanica exoriuntur cum lithosphaera sub amiculum secundum zonam subductionis descendit. Arcibus insularum plerumque augentur continentes.^[1]

Nexus interni

England, Richard W. 2009. "Philip Kearey, Keith A. Klepeis and Frederick J. Vine: Global tectonics." Marine Geophysical Researches 30 (4): 293–4
Frank, F. C. 1968.l "Curvature of Island Arcs." Nature 220 (5165): 363
Hacker, Bradley R., Simon M. Peacock, Geoffrey A. Abers, et Stephen D. Holloway. 2003. "Subduction factory 2. Are intermediate-depth earthquakes in subducting slabs linked to metamorphic dehydration reactions?" Journal of Geophysical Research: Solid Earth 108 (B1): 2030
Isacks, Bryan, Jack Oliver, et Lynn R. Sykes. 1968. "Seismology and the new global tectonics." Journal of Geophysical Research 73, no. 18 (15 Septembris): 5855–99
Oxburgh, E. R., et D. L. Turcotte. 1970. "Thermal Structure of Island Arcs." Geological Society of America Bulletin 81 (6): 1665
Taylor, S. R. 1967. "The origin and growth of continents." Tectonophysics 4 (1): 17–34
Toksöz, M. Nafi. 1975. "The Subduction of the Lithosphere." Scientific American 233 (5): 88–98
Wilson, J., et Tuzo. 1965 "A New Class of Faults and their Bearing on Continental Drift." Nature 207 (4995): 343–47

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