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Bibliographic Details
Main Authors: Pashkina, Valeriya I, Yesikov, Alexander D
Format: Dataset Open Access
Language:en
Published: PANGAEA 1989
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.757607
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author Pashkina, Valeriya I
Yesikov, Alexander D
author_facet Pashkina, Valeriya I
Yesikov, Alexander D
collection Datos científicos de ciencias marinas y ambientales
contents Data on isotopic composition of interstitial and bottom waters collected in an area of gas hydrate occurrence in the Sea of Okhotsk are presented. Investigations indicate that heavy isotopes of oxygen and hydrogen are used in generation of gas hydrate, so that isotopic composition of its water of constitution is: d18O = +1.9 per mil, d2H = +23 per mil (relative to SMOW). Production of authigenic carbonates results in isotopic exchange with interstitial water, which in turn alters its isotopic composition by an increase in d18O. Bottom waters are isotopically light relative to the SMOW standard and to the average isotopic composition of interstitial waters in the area of gas hydrate occurrence in study.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_757607
institution PANGAEA
language en
publishDate 1989
publisher PANGAEA
record_format pangaea
spellingShingle Isotopic composition of bottom and interstitial waters in the area of gas plumes, Sea of Okhotsk
Pashkina, Valeriya I
Yesikov, Alexander D
Archive of Ocean Data; ARCOD; MULT; Multiple investigations; Pisc-1385; Pisc-1389; Pisc-1392; Pisc-1394; Pisc-1395-T-2; Pisc-1403; Pisc-1413; Pisc-1418; Pisc-1418-1; Pisc-1419; Pisc-1423; Sea of Okhotsk; Vulk15-117; Vulk15-119; Vulk15-15; Vulk15-18; Vulk15-20; Vulk15-21; Vulk15-22; Vulk17-56; Vulk17-57; Vulk17-59; Vulk17-63; Vulk17-67
Data on isotopic composition of interstitial and bottom waters collected in an area of gas hydrate occurrence in the Sea of Okhotsk are presented. Investigations indicate that heavy isotopes of oxygen and hydrogen are used in generation of gas hydrate, so that isotopic composition of its water of constitution is: d18O = +1.9 per mil, d2H = +23 per mil (relative to SMOW). Production of authigenic carbonates results in isotopic exchange with interstitial water, which in turn alters its isotopic composition by an increase in d18O. Bottom waters are isotopically light relative to the SMOW standard and to the average isotopic composition of interstitial waters in the area of gas hydrate occurrence in study.
title Isotopic composition of bottom and interstitial waters in the area of gas plumes, Sea of Okhotsk
topic Archive of Ocean Data; ARCOD; MULT; Multiple investigations; Pisc-1385; Pisc-1389; Pisc-1392; Pisc-1394; Pisc-1395-T-2; Pisc-1403; Pisc-1413; Pisc-1418; Pisc-1418-1; Pisc-1419; Pisc-1423; Sea of Okhotsk; Vulk15-117; Vulk15-119; Vulk15-15; Vulk15-18; Vulk15-20; Vulk15-21; Vulk15-22; Vulk17-56; Vulk17-57; Vulk17-59; Vulk17-63; Vulk17-67
url https://doi.org/10.1594/PANGAEA.757607