The geological diversity of island arc volcanism: Northeast Russia |
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| Authors: | V F Belyi |
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| Institution: | (1) Northeastern Institute of Multidisciplinary Research, Far East Division, Russian Academy of Sciences, Magadan, 685000, Russia |
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| Abstract: | Paleovolcanological and paleotectonic reconstructions developed for the continent-ocean transition zone in Northeast Asia demonstrate a high diversity of island arc volcanic settings. There are two main types of island arc volcanism recognized so far, (i) volcanic arcs of euliminary systems (VAES) and (ii) intrageosynclinal volcanic arcs, including areas of insular volcanism (IIV). The volcanic arcs of euliminary systems include the present-day Kuril-Kamchatka, Aleutian, and the Paleozoic- Early Cretaceous Taigonos volcanic arcs. The latter is considered to be a part of the Talovka-Taigonos euliminary system (TTES), an old double island arc system analogous to present-day systems, the Kuril-Kamchatka and Aleutian ones. Both the TTES and similar present-day euliminary systems are structural complexes that confine concentrically-zoned geosyncline areas on the side of the Pacific. The characteristic features of the VAES include a long history of evolution, stable (calc-alkaline) basalt-andesite composition of volcanic products, and transverse geochemical zonation. Geophysical evidence reveals the complicated processes of endogenous crustal accretion and destruction of continental crust within the VAES zones. The IIV follow the structural pattern of the corresponding geosynclinal system. Their evolution is relatively short, while the spatial position and the composition of their magmatic bodies may considerably vary at different stages of evolution of the geosynclinal systems. Most island arc zones are characterized by calc-alkaline volcanism, but potassium alkaline, alkali-ultrabasic, and ultrabasic rocks also occur in some structures. The settings of intrageosynclinal insular volcanism are diverse and include (a) volcanic overcompensation, (b) geoanticlinal uplift, and (c) volcanotectonic downwarping during the orogenic stage of geosynclines. The calc-alkaline volcanism of island environments in geoanticline zones is likely related to the endogenous accretion of continental crust within a geosyncline system. Intrageosynclinal island-arc volcanism is still very poorly understood. Investigation of this phenomenon is one of the urgent tasks of paleovolcanology. |
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