NissirosV1, Main, Exploration, bibRecord, 000335

Gas venting rates from submarine hydrothermal areas around the island of Milos, Hellenic Volcanic Arc

Identifieur interne : 000335 ( Main/Exploration ); précédent : 000334; suivant : 000336

Gas venting rates from submarine hydrothermal areas around the island of Milos, Hellenic Volcanic Arc

Auteurs : P. R. Dando ; J. A. Hughes ; Y. Leahy ; S. J. Niven ; L. J. Taylor ; C. Smith

Source :

Continental Shelf Research [ 0278-4343 ] ; 1995.

RBID : ISTEX:0B709BF188229180372954BD85BF7BE56DDDCC15

English descriptors

Abstract

Abstract: Gas seeps were located, by echo sounding, SCUBA divers and ROV observations, at hydrothermal sites around the island of Milos, in the Hellenic Volcanic Arc. Samples were collected by SCUBA divers and by a ROV from water depths between 3 and 110 m. Fifty-six flow rates from 39 individual seeps were measured and these ranged from 0.2 to 18.51 h−1 at the depth of collection. The major component, 54.9–91.9% of the gas, was carbon dioxide. Hydrogen (≤3%), methane (≤9.7%) and hydrogen sulphide (≤8.1%) were also measured. Hydrothermal free gas fluxes from the submarine hydrothermal areas around Milos were estimated to be greater than 1010 moles y−1. It was concluded that submarine gas seeps along volcanic island arcs may be an important carbon dioxide source.

Url:

https://api.istex.fr/document/0B709BF188229180372954BD85BF7BE56DDDCC15/fulltext/pdf

DOI: 10.1016/0278-4343(95)80002-U

Affiliations:

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Le document en format XML

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<term>Biologiya morya</term>
<term>Black sediment</term>
<term>Carbon dioxide</term>
<term>Clear trend</term>
<term>Continental shelf research</term>
<term>Cosmochimica acta</term>
<term>Cymodocea nodosa</term>
<term>Dando</term>
<term>Diver</term>
<term>East coast</term>
<term>Esmeralda bank</term>
<term>Fault lines</term>
<term>Flow rate</term>
<term>Flow rates</term>
<term>Freshwater research</term>
<term>Fytikas</term>
<term>Geothermal</term>
<term>Geothermal areas</term>
<term>Helium isotopes</term>
<term>Hydrogen content</term>
<term>Hydrogen sulphide</term>
<term>Hydrogen sulphide concentrations</term>
<term>Hydrogen sulphide content</term>
<term>Hydrothermal</term>
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<term>Hydrothermal vents</term>
<term>Individual seeps</term>
<term>Kratemaya bight</term>
<term>Kraternaya bight</term>
<term>Kurile islands</term>
<term>Large areas</term>
<term>Macdonald seamount</term>
<term>Major component</term>
<term>Marine biology</term>
<term>Marine geology</term>
<term>Methane</term>
<term>Methane concentrations</term>
<term>Methane content</term>
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<term>Seabed</term>
<term>Sediment</term>
<term>Sediment column</term>
<term>Sediment temperature</term>
<term>Sediment temperature profiles</term>
<term>Seeps</term>
<term>Southern japan</term>
<term>Spathi</term>
<term>Spathi point</term>
<term>Submarine hydrothermal areas</term>
<term>Submarine hydrothermal areas table</term>
<term>Submarine venting</term>
<term>Sulphide</term>
<term>Temperature measurements</term>
<term>Transect</term>
<term>Transect line</term>
<term>Vent</term>
<term>Vent density</term>
<term>Vent outlet</term>
<term>Vent outlets</term>
<term>Vent temperature</term>
<term>Venting</term>
<term>Venting rates</term>
<term>Volcanic</term>
<term>Volcanic arcs</term>
<term>Volcanic gases</term>
<term>Volcanic island arcs</term>
<term>Water column</term>
<term>Water depth</term>
<term>Water depths</term>
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<term>Yankich island</term>
<term>Zealand journal</term>
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<term>Biologiya morya</term>
<term>Black sediment</term>
<term>Carbon dioxide</term>
<term>Clear trend</term>
<term>Continental shelf research</term>
<term>Cosmochimica acta</term>
<term>Cymodocea nodosa</term>
<term>Dando</term>
<term>Diver</term>
<term>East coast</term>
<term>Esmeralda bank</term>
<term>Fault lines</term>
<term>Flow rate</term>
<term>Flow rates</term>
<term>Freshwater research</term>
<term>Fytikas</term>
<term>Geothermal</term>
<term>Geothermal areas</term>
<term>Helium isotopes</term>
<term>Hydrogen content</term>
<term>Hydrogen sulphide</term>
<term>Hydrogen sulphide concentrations</term>
<term>Hydrogen sulphide content</term>
<term>Hydrothermal</term>
<term>Hydrothermal areas</term>
<term>Hydrothermal vents</term>
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<term>Kraternaya bight</term>
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<term>Large areas</term>
<term>Macdonald seamount</term>
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<term>Marine geology</term>
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<term>Methane concentrations</term>
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<term>Norton sound</term>
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<term>Planetary science letters</term>
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<term>Sediment column</term>
<term>Sediment temperature</term>
<term>Sediment temperature profiles</term>
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<term>Southern japan</term>
<term>Spathi</term>
<term>Spathi point</term>
<term>Submarine hydrothermal areas</term>
<term>Submarine hydrothermal areas table</term>
<term>Submarine venting</term>
<term>Sulphide</term>
<term>Temperature measurements</term>
<term>Transect</term>
<term>Transect line</term>
<term>Vent</term>
<term>Vent density</term>
<term>Vent outlet</term>
<term>Vent outlets</term>
<term>Vent temperature</term>
<term>Venting</term>
<term>Venting rates</term>
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<term>Volcanic arcs</term>
<term>Volcanic gases</term>
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<term>Water column</term>
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<front><div type="abstract" xml:lang="en">Abstract: Gas seeps were located, by echo sounding, SCUBA divers and ROV observations, at hydrothermal sites around the island of Milos, in the Hellenic Volcanic Arc. Samples were collected by SCUBA divers and by a ROV from water depths between 3 and 110 m. Fifty-six flow rates from 39 individual seeps were measured and these ranged from 0.2 to 18.51 h−1 at the depth of collection. The major component, 54.9–91.9% of the gas, was carbon dioxide. Hydrogen (≤3%), methane (≤9.7%) and hydrogen sulphide (≤8.1%) were also measured. Hydrothermal free gas fluxes from the submarine hydrothermal areas around Milos were estimated to be greater than 1010 moles y−1. It was concluded that submarine gas seeps along volcanic island arcs may be an important carbon dioxide source.</div>
</front>
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<name sortKey="Hughes, J A" sort="Hughes, J A" uniqKey="Hughes J" first="J. A." last="Hughes">J. A. Hughes</name>
<name sortKey="Leahy, Y" sort="Leahy, Y" uniqKey="Leahy Y" first="Y." last="Leahy">Y. Leahy</name>
<name sortKey="Niven, S J" sort="Niven, S J" uniqKey="Niven S" first="S. J." last="Niven">S. J. Niven</name>
<name sortKey="Smith, C" sort="Smith, C" uniqKey="Smith C" first="C." last="Smith">C. Smith</name>
<name sortKey="Taylor, L J" sort="Taylor, L J" uniqKey="Taylor L" first="L. J." last="Taylor">L. J. Taylor</name>
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Gas venting rates from submarine hydrothermal areas around the island of Milos, Hellenic Volcanic Arc

Gas venting rates from submarine hydrothermal areas around the island of Milos, Hellenic Volcanic Arc

Source :

English descriptors

Abstract

Links toward previous steps (curation, corpus...)

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

Pour mettre un lien sur cette page dans le réseau Wicri