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The origin of primary magmas beneath the Central Kamchatka Depression by melting of mixed pyroxenite and peridotite source.
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Portnyagin, Maxim , Sobolev A. V., Mironov, N. L. and Hoernle, Kaj (2009) The origin of primary magmas beneath the Central Kamchatka Depression by melting of mixed pyroxenite and peridotite source. [Talk] In: KALMAR - First Bilateral Workshop on Russian-German Cooperation on Kurile-Kamchatka and Aleutean Marginal Sea-Island Arc Systems. , 27.04.-01.05, Petropavlovsk-Kamchatsky, Russia .
Full text not available from this repository.Document Type: | Conference or Workshop Item (Talk) |
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Keywords: | KALMAR |
Research affiliation: | OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-MUHS Magmatic and Hydrothermal Systems |
Refereed: | No |
Date Deposited: | 25 Nov 2009 15:22 |
Last Modified: | 23 Feb 2012 05:10 |
URI: | https://oceanrep.geomar.de/id/eprint/5341 |
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