NissirosV1, Istex, Corpus, bibRecord, 000151

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

Identifieur interne : 000151 ( Istex/Corpus ); précédent : 000150; suivant : 000152

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

Links to Exploration step

ISTEX:0B709BF188229180372954BD85BF7BE56DDDCC15

Le document en format XML

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<head><ce:title>Gas venting rates from submarine hydrothermal areas around the island of Milos, Hellenic Volcanic Arc</ce:title>
<ce:author-group><ce:author><ce:given-name>P.R.</ce:given-name>
<ce:surname>Dando</ce:surname>
<ce:cross-ref refid="FN1"><ce:sup>∗</ce:sup>
</ce:cross-ref>
<ce:cross-ref refid="FN2"><ce:sup>↼</ce:sup>
</ce:cross-ref>
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<ce:author><ce:given-name>J.A.</ce:given-name>
<ce:surname>Hughes</ce:surname>
<ce:cross-ref refid="FN3"><ce:sup>†</ce:sup>
</ce:cross-ref>
</ce:author>
<ce:author><ce:given-name>Y.</ce:given-name>
<ce:surname>Leahy</ce:surname>
<ce:cross-ref refid="FN3"><ce:sup>†</ce:sup>
</ce:cross-ref>
</ce:author>
<ce:author><ce:given-name>S.J.</ce:given-name>
<ce:surname>Niven</ce:surname>
<ce:cross-ref refid="FN1"><ce:sup>∗</ce:sup>
</ce:cross-ref>
</ce:author>
<ce:author><ce:given-name>L.J.</ce:given-name>
<ce:surname>Taylor</ce:surname>
<ce:cross-ref refid="FN1"><ce:sup>∗</ce:sup>
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</ce:author>
<ce:author><ce:given-name>C.</ce:given-name>
<ce:surname>Smith</ce:surname>
<ce:cross-ref refid="FN3"><ce:sup>†</ce:sup>
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<ce:footnote id="FN1"><ce:label>∗</ce:label>
<ce:note-para>Marine Biological Association of the United Kingdom, Citadel Hill, Plymouth, PL1 2PB, U.K.</ce:note-para>
</ce:footnote>
<ce:footnote id="FN2"><ce:label>↼</ce:label>
<ce:note-para>Present address: School of Ocean Sciences, University College of North Wales, Gwynedd, LL59 5EY, U.K.</ce:note-para>
</ce:footnote>
<ce:footnote id="FN3"><ce:label>†</ce:label>
<ce:note-para>Institute of Marine Biology of Crete, P.O. Box 2214, 710 03 Iraklion, Crete, Greece.</ce:note-para>
</ce:footnote>
</ce:author-group>
<ce:date-received day="1" month="6" year="1993"></ce:date-received>
<ce:date-revised day="22" month="2" year="1994"></ce:date-revised>
<ce:date-accepted day="26" month="5" year="1994"></ce:date-accepted>
<ce:abstract><ce:section-title>Abstract</ce:section-title>
<ce:abstract-sec><ce:simple-para>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<ce:sup>−1</ce:sup>
 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 10<ce:sup>10</ce:sup>
 moles y<ce:sup>−1</ce:sup>
. It was concluded that submarine gas seeps along volcanic island arcs may be an important carbon dioxide source.</ce:simple-para>
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<abstract 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.</abstract>
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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

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