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Giant caldera in the Arctic Ocean: Evidence of the catastrophic eruptive event. / Piskarev, A.; Elkina, D.

в: Scientific Reports, Том 7, 46248, 2017.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Piskarev, A & Elkina, D 2017, 'Giant caldera in the Arctic Ocean: Evidence of the catastrophic eruptive event', Scientific Reports, Том. 7, 46248. https://doi.org/10.1038/srep46248

APA

Piskarev, A., & Elkina, D. (2017). Giant caldera in the Arctic Ocean: Evidence of the catastrophic eruptive event. Scientific Reports, 7, [46248]. https://doi.org/10.1038/srep46248

Vancouver

Piskarev A, Elkina D. Giant caldera in the Arctic Ocean: Evidence of the catastrophic eruptive event. Scientific Reports. 2017;7. 46248. https://doi.org/10.1038/srep46248

Author

Piskarev, A. ; Elkina, D. / Giant caldera in the Arctic Ocean: Evidence of the catastrophic eruptive event. в: Scientific Reports. 2017 ; Том 7.

BibTeX

@article{0216f42e549a4d7b9c45f9d27f501627,
title = "Giant caldera in the Arctic Ocean: Evidence of the catastrophic eruptive event",
abstract = "A giant caldera located in the eastern segment of the Gakkel Ridge could be firstly seen on the bathymetric map of the Arctic Ocean published in 1999. In 2014, seismic and multibeam echosounding data were acquired at the location. The caldera is 80 km long, 40 km wide and 1.2 km deep. The total volume of ejected volcanic material is estimated as no less than 3000 km3 placing it into the same category with the largest Quaternary calderas (Yellowstone and Toba). Time of the eruption is estimated as ~ 1.1 Ma. Thin layers of the volcanic material related to the eruption had been identified in sedimentary cores located about 1000 km away from the Gakkel Ridge. The Gakkel Ridge Caldera is the single example of a supervolcano in the rift zone of the Mid-Oceanic Ridge System.",
author = "A. Piskarev and D Elkina",
year = "2017",
doi = "10.1038/srep46248",
language = "English",
volume = "7",
journal = "Scientific Reports",
issn = "2045-2322",
publisher = "Nature Publishing Group",

}

RIS

TY - JOUR

T1 - Giant caldera in the Arctic Ocean: Evidence of the catastrophic eruptive event

AU - Piskarev, A.

AU - Elkina, D

PY - 2017

Y1 - 2017

N2 - A giant caldera located in the eastern segment of the Gakkel Ridge could be firstly seen on the bathymetric map of the Arctic Ocean published in 1999. In 2014, seismic and multibeam echosounding data were acquired at the location. The caldera is 80 km long, 40 km wide and 1.2 km deep. The total volume of ejected volcanic material is estimated as no less than 3000 km3 placing it into the same category with the largest Quaternary calderas (Yellowstone and Toba). Time of the eruption is estimated as ~ 1.1 Ma. Thin layers of the volcanic material related to the eruption had been identified in sedimentary cores located about 1000 km away from the Gakkel Ridge. The Gakkel Ridge Caldera is the single example of a supervolcano in the rift zone of the Mid-Oceanic Ridge System.

AB - A giant caldera located in the eastern segment of the Gakkel Ridge could be firstly seen on the bathymetric map of the Arctic Ocean published in 1999. In 2014, seismic and multibeam echosounding data were acquired at the location. The caldera is 80 km long, 40 km wide and 1.2 km deep. The total volume of ejected volcanic material is estimated as no less than 3000 km3 placing it into the same category with the largest Quaternary calderas (Yellowstone and Toba). Time of the eruption is estimated as ~ 1.1 Ma. Thin layers of the volcanic material related to the eruption had been identified in sedimentary cores located about 1000 km away from the Gakkel Ridge. The Gakkel Ridge Caldera is the single example of a supervolcano in the rift zone of the Mid-Oceanic Ridge System.

UR - https://www.nature.com/articles/srep46248

U2 - 10.1038/srep46248

DO - 10.1038/srep46248

M3 - Article

VL - 7

JO - Scientific Reports

JF - Scientific Reports

SN - 2045-2322

M1 - 46248

ER -

ID: 7743427