Late Pleistocene-Holocene Volcanism on the Kamchatka Peninsula, Northwest Pacific Region
Late Pleistocene-Holocene volcanism in Kamchatka results from the subduction of the Pacific Plate under the peninsula and forms three volcanic belts arranged in en echelon manner from southeast to northwest. The cross-arc extent of recent volcanism exceeds 250 km and is one of the widest worldwide....
Main Authors: | , , , , , |
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Format: | Text |
Language: | English |
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American Geophysical Union
2007
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Online Access: | http://repo.kscnet.ru/1039/ http://repo.kscnet.ru/1039/1/Ponomareva%202007.pdf http://onlinelibrary.wiley.com/doi/10.1029/172GM15 |