Petrological study of monogenetic volcanoes in the fore-arc region of the northern Kamchatka Peninsula

The western part of the Pacific Plate is subducting under the Okhotsk Plate along Kuril-Kamchatka Trench, and the northern part of it is subducting under the Bering Sea Plate with high obliquity along the western Aleutians arc. The three plates form the Aleutian-Kamchatka triple junction (Eichelberg...

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Bibliographic Details
Main Authors: Nishizawa Tatsuji, Churikova Tatiana, Gordeychik Boris, Ishizuka Osamu, Nakamura Hitomi, Iwamori Hikaru
Format: Text
Language:English
Published: Japan Geoscience Union 2014
Subjects:
38.33.15 Геохимия отдельных элементов
38.33.19 Геохимия природных вод и рассолов
Bering Sea
Kamchatka Peninsula
Okhotsk
Pacific
Kamchatka
Online Access:http://repo.kscnet.ru/3045/
http://repo.kscnet.ru/3045/1/Nishizawa_2014%20JPGU.pdf
http://www2.jpgu.org/meeting/2014/session/PDF/S-VC54/SVC54-02_e.pdf
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Summary:The western part of the Pacific Plate is subducting under the Okhotsk Plate along Kuril-Kamchatka Trench, and the northern part of it is subducting under the Bering Sea Plate with high obliquity along the western Aleutians arc. The three plates form the Aleutian-Kamchatka triple junction (Eichelberger et al., 2013). The northern edge of the Pacific Plate is separated from Bering Sea Plate by transform fault, and the mantle edge beneath the Kamchatka Peninsula is thought to be open towards the Bering Sea.

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