Standard

Gas hydrate accumulation at the Hakon Mosby Mud Volcano. / Ginsburg, GD; Milkov, AV; Soloviev, VA; Cherkashev, GA; Vogt, PR; Crane, K; Lorenson, TD; Khutorskoy, MD.

In: Geo-Marine Letters, Vol. 19, No. 1-2, 09.1999, p. 57-67.

Research output: Contribution to journal › Article › peer-review

Harvard

Ginsburg, GD, Milkov, AV, Soloviev, VA, Cherkashev, GA, Vogt, PR, Crane, K, Lorenson, TD & Khutorskoy, MD 1999, 'Gas hydrate accumulation at the Hakon Mosby Mud Volcano', Geo-Marine Letters, vol. 19, no. 1-2, pp. 57-67. https://doi.org/10.1007/s003670050093

APA

Ginsburg, GD., Milkov, AV., Soloviev, VA., Cherkashev, GA., Vogt, PR., Crane, K., Lorenson, TD., & Khutorskoy, MD. (1999). Gas hydrate accumulation at the Hakon Mosby Mud Volcano. Geo-Marine Letters, 19(1-2), 57-67. https://doi.org/10.1007/s003670050093

Vancouver

Ginsburg GD, Milkov AV, Soloviev VA, Cherkashev GA, Vogt PR, Crane K et al. Gas hydrate accumulation at the Hakon Mosby Mud Volcano. Geo-Marine Letters. 1999 Sep;19(1-2):57-67. https://doi.org/10.1007/s003670050093

Author

Ginsburg, GD ; Milkov, AV ; Soloviev, VA ; Cherkashev, GA ; Vogt, PR ; Crane, K ; Lorenson, TD ; Khutorskoy, MD. / Gas hydrate accumulation at the Hakon Mosby Mud Volcano. In: Geo-Marine Letters. 1999 ; Vol. 19, No. 1-2. pp. 57-67.

BibTeX

@article{e25927d3424a4453aa41971951b68452,
title = "Gas hydrate accumulation at the Hakon Mosby Mud Volcano",
abstract = "Gas hydrate (GH) accumulation is characterized and modeled, for the Hakon Mosby mud volcano, ca. 1.5 km across, located on the Norway-Barents-Svalbard margin. Pore water chemical and isotopic results based on shallow sediment cores as well as geothermal and geomorphological data suggest that the GH accumulation is of a concentric pattern controlled by and formed essentially from the ascending mud volcano fluid. The gas hydrate content of sediment peaks at 25% by volume, averaging about 1.2% throughout the accumulation. The amount of hydrate methane is estimated at ca. 10(8) m(3) STP, which could account for about 1-10% of the gas that has escaped from the volcano since its origin.",
keywords = "WATER",
author = "GD Ginsburg and AV Milkov and VA Soloviev and GA Cherkashev and PR Vogt and K Crane and TD Lorenson and MD Khutorskoy",
year = "1999",
month = sep,
doi = "10.1007/s003670050093",
language = "Английский",
volume = "19",
pages = "57--67",
journal = "Geo-Marine Letters",
issn = "0276-0460",
publisher = "Springer Nature",
number = "1-2",

}

RIS

TY - JOUR

T1 - Gas hydrate accumulation at the Hakon Mosby Mud Volcano

AU - Ginsburg, GD

AU - Milkov, AV

AU - Soloviev, VA

AU - Cherkashev, GA

AU - Vogt, PR

AU - Crane, K

AU - Lorenson, TD

AU - Khutorskoy, MD

PY - 1999/9

Y1 - 1999/9

N2 - Gas hydrate (GH) accumulation is characterized and modeled, for the Hakon Mosby mud volcano, ca. 1.5 km across, located on the Norway-Barents-Svalbard margin. Pore water chemical and isotopic results based on shallow sediment cores as well as geothermal and geomorphological data suggest that the GH accumulation is of a concentric pattern controlled by and formed essentially from the ascending mud volcano fluid. The gas hydrate content of sediment peaks at 25% by volume, averaging about 1.2% throughout the accumulation. The amount of hydrate methane is estimated at ca. 10(8) m(3) STP, which could account for about 1-10% of the gas that has escaped from the volcano since its origin.

AB - Gas hydrate (GH) accumulation is characterized and modeled, for the Hakon Mosby mud volcano, ca. 1.5 km across, located on the Norway-Barents-Svalbard margin. Pore water chemical and isotopic results based on shallow sediment cores as well as geothermal and geomorphological data suggest that the GH accumulation is of a concentric pattern controlled by and formed essentially from the ascending mud volcano fluid. The gas hydrate content of sediment peaks at 25% by volume, averaging about 1.2% throughout the accumulation. The amount of hydrate methane is estimated at ca. 10(8) m(3) STP, which could account for about 1-10% of the gas that has escaped from the volcano since its origin.

KW - WATER

U2 - 10.1007/s003670050093

DO - 10.1007/s003670050093

M3 - статья

VL - 19

SP - 57

EP - 67

JO - Geo-Marine Letters

JF - Geo-Marine Letters

SN - 0276-0460

IS - 1-2

ER -

ID: 35934060