Chemical and isotopic compositions of authigenic carbonates from the area of the Sakhalin-Deryugin gas anomaly, Sea of Okhotsk

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Auteurs principaux: Obzhirov, Anatoly I, Astakhov, Anatolii S, Astakhova, N V
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2000
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author Obzhirov, Anatoly I
Astakhov, Anatolii S
Astakhova, N V
author_facet Obzhirov, Anatoly I
Astakhov, Anatolii S
Astakhova, N V
collection Datos científicos de ciencias marinas y ambientales
contents Features of sedimentation of carbonate mineral associations in the northeastern shelf of Sakhalin and other regions of the Sea of Okhotsk are considered. Special attention is paid to correlation between carbonate neoformations and abnormal fluxes of methane. In bottom sediments with high contents of methane carbonate-sulfide associations occur, their generation has been influenced by gas (mostly methane) fields. Joint consideration of distribution of gas and geochemical fields and mineral associations in the Sea of Okhotsk allows to understand better a mechanism of mineral generation in bottom sediments, possible formation of ore accumulations, and to use them as indicators for prognosis of mineral resources.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_761748
institution PANGAEA
language en
publishDate 2000
publisher PANGAEA
record_format pangaea
spellingShingle Chemical and isotopic compositions of authigenic carbonates from the area of the Sakhalin-Deryugin gas anomaly, Sea of Okhotsk
Obzhirov, Anatoly I
Astakhov, Anatolii S
Astakhova, N V
Akademik A Nesmeyanov; Akademik M.A. Lavrentyev; AN_1993; AN25-936; Archive of Ocean Data; ARCOD; BC; Box corer; GC; Gravity corer; LV27/GREGORY; LV27-1; LV27-1A; LV27-2; MULT; Multiple investigations; Obzh-82156; Obzh-89228; Obzh-9312; Sea of Okhotsk
Features of sedimentation of carbonate mineral associations in the northeastern shelf of Sakhalin and other regions of the Sea of Okhotsk are considered. Special attention is paid to correlation between carbonate neoformations and abnormal fluxes of methane. In bottom sediments with high contents of methane carbonate-sulfide associations occur, their generation has been influenced by gas (mostly methane) fields. Joint consideration of distribution of gas and geochemical fields and mineral associations in the Sea of Okhotsk allows to understand better a mechanism of mineral generation in bottom sediments, possible formation of ore accumulations, and to use them as indicators for prognosis of mineral resources.
title Chemical and isotopic compositions of authigenic carbonates from the area of the Sakhalin-Deryugin gas anomaly, Sea of Okhotsk
topic Akademik A Nesmeyanov; Akademik M.A. Lavrentyev; AN_1993; AN25-936; Archive of Ocean Data; ARCOD; BC; Box corer; GC; Gravity corer; LV27/GREGORY; LV27-1; LV27-1A; LV27-2; MULT; Multiple investigations; Obzh-82156; Obzh-89228; Obzh-9312; Sea of Okhotsk
url https://doi.org/10.1594/PANGAEA.761748