The abundance of mercury in rocks, minerals and native sulphur by a microwave-excited argon plasma
Identifieur interne : 000543 ( Main/Exploration ); précédent : 000542; suivant : 000544The abundance of mercury in rocks, minerals and native sulphur by a microwave-excited argon plasma
Auteurs : R. K. Srivastava [Inde]Source :
- Chemical Geology [ 0009-2541 ] ; 1979.
Descripteurs français
- Wicri :
- topic : Soufre.
English descriptors
- KwdEn :
- Amphibolite hornblende, Argon plasma, Average content, Basalt, Basaltic rocks, Basic rocks, Biotite, Black forest, Central massif, Clay minerals, Content show, Continental ones, Different parts, Early crystallates, Gabbroid magmas, Granite, Granitic, Granitic rocks, Great britain, Greece sulphur, Hawaii sulphur, Hornblende, Igneous rocks, Kameni, Kameni island, Kameni island greece sulphur, Large number, Magma, Main stage, Mercury content, Mineral locality, Native sulphur, Oceanic volcanism, Other hand, Present data, Primary sulphurs, Same locality, Seawater sulphates, Silicate minerals, Solfataras, Standard deviation, Sulphur, Sulphur samples.
- Teeft :
- Amphibolite hornblende, Argon plasma, Average content, Basalt, Basaltic rocks, Basic rocks, Biotite, Black forest, Central massif, Clay minerals, Content show, Continental ones, Different parts, Early crystallates, Gabbroid magmas, Granite, Granitic, Granitic rocks, Great britain, Greece sulphur, Hawaii sulphur, Hornblende, Igneous rocks, Kameni, Kameni island, Kameni island greece sulphur, Large number, Magma, Main stage, Mercury content, Mineral locality, Native sulphur, Oceanic volcanism, Other hand, Present data, Primary sulphurs, Same locality, Seawater sulphates, Silicate minerals, Solfataras, Standard deviation, Sulphur, Sulphur samples.
Abstract
Abstract: Igneous rocks, silicate minerals and native sulphur have been analysed for their mercury content by a microwave-excited argon plasma. Basic and ultrabasic igneous rocks have abundances between 3 and 31 ppb Hg. The granitic rocks show much larger variations. The content in the silicate minerals is highly variable, ranging from less than 1 ppb Hg in an igneous biotite to 55 ppb Hg in a pegmatitic biotite. The analysed clay minerals give 110 and 200 ppb Hg. Volcanic elemental S contain from 11 to 9300 ppb Hg, the values on the lower side being from oceanic volcanoes and on the higher side for continental or marginal volcanoes.
Url:
DOI: 10.1016/0009-2541(79)90043-3
Affiliations:
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K." last="Srivastava">R. K. Srivastava</name><affiliation wicri:level="1"><country xml:lang="fr">Inde</country><wicri:regionArea>Department of Geology, University of Rajasthan</wicri:regionArea><wicri:noRegion>University of Rajasthan</wicri:noRegion></affiliation></author></analytic><monogr></monogr><series><title level="j">Chemical Geology</title><title level="j" type="abbrev">CHEMGE</title><idno type="ISSN">0009-2541</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1979">1979</date><biblScope unit="volume">27</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="255">255</biblScope><biblScope unit="page" to="263">263</biblScope></imprint><idno type="ISSN">0009-2541</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0009-2541</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Amphibolite hornblende</term><term>Argon plasma</term><term>Average content</term><term>Basalt</term><term>Basaltic rocks</term><term>Basic rocks</term><term>Biotite</term><term>Black forest</term><term>Central massif</term><term>Clay minerals</term><term>Content show</term><term>Continental ones</term><term>Different parts</term><term>Early crystallates</term><term>Gabbroid magmas</term><term>Granite</term><term>Granitic</term><term>Granitic rocks</term><term>Great britain</term><term>Greece sulphur</term><term>Hawaii sulphur</term><term>Hornblende</term><term>Igneous rocks</term><term>Kameni</term><term>Kameni island</term><term>Kameni island greece sulphur</term><term>Large number</term><term>Magma</term><term>Main stage</term><term>Mercury content</term><term>Mineral locality</term><term>Native sulphur</term><term>Oceanic volcanism</term><term>Other hand</term><term>Present data</term><term>Primary sulphurs</term><term>Same locality</term><term>Seawater sulphates</term><term>Silicate minerals</term><term>Solfataras</term><term>Standard deviation</term><term>Sulphur</term><term>Sulphur samples</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Amphibolite hornblende</term><term>Argon plasma</term><term>Average content</term><term>Basalt</term><term>Basaltic rocks</term><term>Basic rocks</term><term>Biotite</term><term>Black forest</term><term>Central massif</term><term>Clay minerals</term><term>Content show</term><term>Continental ones</term><term>Different parts</term><term>Early crystallates</term><term>Gabbroid magmas</term><term>Granite</term><term>Granitic</term><term>Granitic rocks</term><term>Great britain</term><term>Greece sulphur</term><term>Hawaii sulphur</term><term>Hornblende</term><term>Igneous rocks</term><term>Kameni</term><term>Kameni island</term><term>Kameni island greece sulphur</term><term>Large number</term><term>Magma</term><term>Main stage</term><term>Mercury content</term><term>Mineral locality</term><term>Native sulphur</term><term>Oceanic volcanism</term><term>Other hand</term><term>Present data</term><term>Primary sulphurs</term><term>Same locality</term><term>Seawater sulphates</term><term>Silicate minerals</term><term>Solfataras</term><term>Standard deviation</term><term>Sulphur</term><term>Sulphur samples</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Soufre</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Igneous rocks, silicate minerals and native sulphur have been analysed for their mercury content by a microwave-excited argon plasma. Basic and ultrabasic igneous rocks have abundances between 3 and 31 ppb Hg. The granitic rocks show much larger variations. The content in the silicate minerals is highly variable, ranging from less than 1 ppb Hg in an igneous biotite to 55 ppb Hg in a pegmatitic biotite. The analysed clay minerals give 110 and 200 ppb Hg. Volcanic elemental S contain from 11 to 9300 ppb Hg, the values on the lower side being from oceanic volcanoes and on the higher side for continental or marginal volcanoes.</div></front></TEI><affiliations><list><country><li>Inde</li></country></list><tree><country name="Inde"><noRegion><name sortKey="Srivastava, R K" sort="Srivastava, R K" uniqKey="Srivastava R" first="R. K." last="Srivastava">R. K. Srivastava</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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