Sakhalin Island Arc: Difference between revisions

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Sakhalin Island Arc is an ancient volcanic arc dating from the Early Miocene.^[1] The arc was a result of the Okhotsk Plate subducting beneath the Eurasian Plate in the convergence zone. The arc runs from mainland Asia through Sakhalin Island into central Hokkaido and the collision zone around the Daisetsuzan Volcanic Group, where the Kuril Island Arc and the Northeastern Japan Arc meet.

References

^ Ivanov, Andrey (March 27, 2003). "18 The Far East". In Shahgedanova, Maria (ed.). The Physical Geography of Northern Eurasia. Oxford Regional Environments. Vol. 3. Google Books: Oxford University Press. pp. 428–429. ISBN 978-0-19-823384-8. Retrieved 2008-07-16.

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[FarEast-1] Ivanov, Andrey (March 27, 2003). "18 The Far East". In Shahgedanova, Maria (ed.). The Physical Geography of Northern Eurasia. Oxford Regional Environments. Vol. 3. Google Books: Oxford University Press. pp. 428–429. ISBN 978-0-19-823384-8. Retrieved 2008-07-16.

[1]

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+{{Coord missing|Sakhalin Oblast|Japan}}
-'''Sakhalin Island Arc''' is an ancient [[volcanic arc]] dating from the [[Early Miocene]].<ref name="FarEast">{{cite book|last=Ivanov|first=Andrey |title=The Physical Geography of Northern Eurasia|editor=Shahgedanova, Maria|publisher=Oxford University Press|location=Google Books|date=March 27, 2003|series=Oxford Regional Environments|volume=3|pages=428–429|chapter=18 The Far East|isbn=978-0-19-823384-8 |url=https://books.google.com/books?id=8CFiT3qbN5UC&pg=PA428&lpg=PA428&dq=sakhalin+arc&source=web&ots=6VjcSD1zqG&sig=1IUPEQJeZUM4thJ5WYGfbzJfW54&hl=en&sa=X&oi=book_result&resnum=8&ct=result#PPA428,M1|accessdate=2008-07-16}}</ref> The arc was a result of the [[Okhotsk Plate]] subducting beneath the [[Eurasian Plate]] in the [[Convergent boundary|convergence]] zone. The arc runs from mainland [[Asia]] through [[Sakhalin Island]] into central [[Hokkaido]] and the collision zone around the [[Daisetsuzan Volcanic Group]], where the [[Kuril Islands|Kuril Island Arc]] and the [[Northeastern Japan Arc]] meet.
+'''Sakhalin Island Arc''' is an ancient [[volcanic arc]] dating from the [[Early Miocene]].<ref name="FarEast">{{cite book|last=Ivanov|first=Andrey |title=The Physical Geography of Northern Eurasia|editor=Shahgedanova, Maria|publisher=Oxford University Press|location=Google Books|date=March 27, 2003|series=Oxford Regional Environments|volume=3|pages=428–429|chapter=18 The Far East|isbn=978-0-19-823384-8 |url=https://books.google.com/books?id=8CFiT3qbN5UC&pg=PA428&lpg=PA428&dq=sakhalin+arc&source=web&ots=6VjcSD1zqG&sig=1IUPEQJeZUM4thJ5WYGfbzJfW54&hl=en&sa=X&oi=book_result&resnum=8&ct=result#PPA428,M1|accessdate=2008-07-16}}</ref> The arc was a result of the [[Okhotsk Plate]] subducting beneath the [[Eurasian Plate]] in the [[Convergent boundary|convergence]] zone. The arc runs from mainland [[Asia]] through [[Sakhalin|Sakhalin Island]] into central [[Hokkaido]] and the collision zone around the [[Daisetsuzan Volcanic Group]], where the [[Kuril Islands|Kuril Island Arc]] and the [[Northeastern Japan Arc]] meet.
 ==References==
 {{reflist}}
-{{coord missing|Sakhalin Oblast|Japan}}
 [[Category:Volcanic arcs]]
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 {{FarEast-Russia-geo-stub}}
-{{SakhalinOblast-geo-stub}}
 {{Hokkaido-geo-stub}}
+{{SakhalinOblast-geo-stub}}