| dc.contributor.author |
Nishizawa T. |
|
| dc.contributor.author |
Churikova T.G. |
|
| dc.contributor.author |
Gordeychik B.N. |
|
| dc.contributor.author |
Ishizuka O. |
|
| dc.contributor.author |
Nakamura H. |
|
| dc.contributor.author |
Iwamori H. |
|
| dc.date.accessioned |
2019-09-03T05:55:38Z |
|
| dc.date.available |
2019-09-03T05:55:38Z |
|
| dc.date.issued |
2014-02-28 |
|
| dc.identifier |
http://repo.kscnet.ru/3044/ |
|
| dc.identifier |
http://repo.kscnet.ru/3044/1/Nishizawa_2014 Geofluid.pdf |
|
| dc.identifier.citation |
Nishizawa T., Churikova T.G., Gordeychik B.N., Ishizuka O., Nakamura H., Iwamori H. (2014) Petrological study of monogenetic volcanoes in the fore-arc region of the northern Kamchatka Peninsula // Geofluid-3. Nature and Dynamics of fluids in Subduction Zones. Tokyo, Japan, February 28 - March 3, 2014 . Tokyo, Japan: Tokyo Institute of Technology. С. 116. |
|
| dc.identifier.uri |
https://repository.geologyscience.ru/handle/123456789/5838 |
|
| dc.description.abstract |
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 [l]. 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. |
|
| dc.language.iso |
en |
|
| dc.publisher |
Tokyo Institute of Technology |
|
| dc.subject |
38.33.15 Геохимия отдельных элементов |
|
| dc.subject |
38.33.17 Геохимия природных процессов |
|
| dc.title |
Petrological study of monogenetic volcanoes in the fore-arc region of the northern Kamchatka Peninsula |
|
| dc.type |
Раздел книги |
|