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The isotopic composition of subduction fluid: High-, low-, or normal δ^(18)O?
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The isotopic composition of subduction fluid: High-, low-, or normal δ^(18)O?
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Identification of Source Lithology at South Segment of Kamchatka Subduction Zone
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Amphibole record of 1964 plinian and following dome-forming eruptions of Shivelu...
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BERING - A new international marine research project to investigate the magmatic...
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Petrology and geochemistry of plutonic rocks in the Northwest Pacific Ocean and...
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First identification of cryptotephra from Kamchatka in a Greenland ice core and...
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A Kamchatka volcanic time-synchronous layer links East Asia to East Coast North...
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Small but important: new data about activity and composition of Zarechny volcano...
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Reprint of Silicate-sulfide liquid immiscibility in modern arc basalt (Tolbachik...
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Silicate-sulfide liquid immiscibility in modern arc basalt (Tolbachik volcano, K...
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Silicate-sulfide liquid immiscibility in modern arc basalt (Tolbachik volcano, K...
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Volcanic activity at Sedankinsky Dol lava field, Sredinny Ridge, during the Holo...
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Towards a Kamchatka tephrochronological framework for testing synchronous climat...
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SO-249 BERING – Origin and Evolution of the Bering Sea: An Integrated Geochronol...
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Oxygen isotope evidence for slab melting in modern and ancient subduction zones
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Coseismic coastal subsidence associated with unusually wide rupture of prehistor...
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Application of Tephrochronology in the Kurile-Kamchatka and Aleutean Marginal Se...
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Northwest Pacific ice-rafted debris at 38 degrees N reveals episodic ice-sheet c...
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Northwest Pacific ice-rafted debris at 38◦N reveals episodic ice-sheet change in...
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38.37.25 Вулканология
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