Clay minerals in sediments from contact zones with basalt sills

Clay minerals (fraction

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Литология и полезные ископаемые 2019-05 (3), p.234-247
Hauptverfasser: Kurnosov, V. B., Sakharov, B. A., Geptner, A. R., Konovalov, Yu. I., Goncharov, E. O.
Format: Artikel
Sprache:eng
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 247
container_issue 3
container_start_page 234
container_title Литология и полезные ископаемые
container_volume
creator Kurnosov, V. B.
Sakharov, B. A.
Geptner, A. R.
Konovalov, Yu. I.
Goncharov, E. O.
description Clay minerals (fraction
doi_str_mv 10.31857/S0024-497X20193234-247
format Article
fullrecord <record><control><sourceid>crossref</sourceid><recordid>TN_cdi_crossref_primary_10_31857_S0024_497X20193234_247</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>10_31857_S0024_497X20193234_247</sourcerecordid><originalsourceid>FETCH-LOGICAL-c977-c171d27e88ba9748b9c9ac8b1447e5b3d49130d5ca21eeda8aac5dd8ef3ed60c3</originalsourceid><addsrcrecordid>eNpNz0tLAzEUBeAsFCy1v8H8gdG8xiQrkcEXFLqwC3fhJrmDgXlI7oDUX2-pIq4OHDgHPsaupLjW0rX25lUIZRrj7ZsS0mulTaOMPWOrv_6CbYhKFFIpL5VWK3bXDXDgY5mwwkC8TJwwlxGnhXhf55GneVogLfxrnpD4Z1neeQSCYeFUhoEu2Xl_HOLmN9ds__iw756b7e7ppbvfNslb2yRpZVYWnYvgrXHRJw_JRWmMxTbqbLzUIrcJlETM4ABSm7PDXmO-FUmvmf25TXUmqtiHj1pGqIcgRTjpw0kf_uvDUa-_ATyoUPY</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Clay minerals in sediments from contact zones with basalt sills</title><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><creator>Kurnosov, V. B. ; Sakharov, B. A. ; Geptner, A. R. ; Konovalov, Yu. I. ; Goncharov, E. O.</creator><creatorcontrib>Kurnosov, V. B. ; Sakharov, B. A. ; Geptner, A. R. ; Konovalov, Yu. I. ; Goncharov, E. O.</creatorcontrib><description>Clay minerals (fraction &lt;0.001 mm) of Upper Pleistocene clayey-sandy-silty sediments recovered by DSDP Holes 481 and 481A in the Northern Trough, Guaymas Basin, Gulf of California, were studied by X-ray based on the modeling of diffraction patterns and their comparison with experimental diffractograms. Terrigenous clay minerals are represented mainly by dioctahedral micaceous varieties (mixed-layer disordered illite-smectites, illite) with the chlorite admixture and by kaolinite in the upper section of unaltered sediments. Intrusion of hot basalt sills (total thickness of the complex is about 27 m) provoked alterations in the phase composition of clay minerals in sediments (7.5 m thick) overlying the sill complex. These sediments include newly formed triooctahedral layered silicates (mixed-layer chlorite-smectites, smectite). Sediments inside the sill complex include trioctahedral mixed-layer mica-smtctite-vermiculite or trioctahedral smectite. The trioctahedral mixed-layer chlorite-smectite coexisting with smectite was found in a single sample of the same complex.</description><identifier>ISSN: 0024-497X</identifier><identifier>DOI: 10.31857/S0024-497X20193234-247</identifier><language>eng</language><ispartof>Литология и полезные ископаемые, 2019-05 (3), p.234-247</ispartof><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,781,785,27928,27929</link.rule.ids></links><search><creatorcontrib>Kurnosov, V. B.</creatorcontrib><creatorcontrib>Sakharov, B. A.</creatorcontrib><creatorcontrib>Geptner, A. R.</creatorcontrib><creatorcontrib>Konovalov, Yu. I.</creatorcontrib><creatorcontrib>Goncharov, E. O.</creatorcontrib><title>Clay minerals in sediments from contact zones with basalt sills</title><title>Литология и полезные ископаемые</title><description>Clay minerals (fraction &lt;0.001 mm) of Upper Pleistocene clayey-sandy-silty sediments recovered by DSDP Holes 481 and 481A in the Northern Trough, Guaymas Basin, Gulf of California, were studied by X-ray based on the modeling of diffraction patterns and their comparison with experimental diffractograms. Terrigenous clay minerals are represented mainly by dioctahedral micaceous varieties (mixed-layer disordered illite-smectites, illite) with the chlorite admixture and by kaolinite in the upper section of unaltered sediments. Intrusion of hot basalt sills (total thickness of the complex is about 27 m) provoked alterations in the phase composition of clay minerals in sediments (7.5 m thick) overlying the sill complex. These sediments include newly formed triooctahedral layered silicates (mixed-layer chlorite-smectites, smectite). Sediments inside the sill complex include trioctahedral mixed-layer mica-smtctite-vermiculite or trioctahedral smectite. The trioctahedral mixed-layer chlorite-smectite coexisting with smectite was found in a single sample of the same complex.</description><issn>0024-497X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><recordid>eNpNz0tLAzEUBeAsFCy1v8H8gdG8xiQrkcEXFLqwC3fhJrmDgXlI7oDUX2-pIq4OHDgHPsaupLjW0rX25lUIZRrj7ZsS0mulTaOMPWOrv_6CbYhKFFIpL5VWK3bXDXDgY5mwwkC8TJwwlxGnhXhf55GneVogLfxrnpD4Z1neeQSCYeFUhoEu2Xl_HOLmN9ds__iw756b7e7ppbvfNslb2yRpZVYWnYvgrXHRJw_JRWmMxTbqbLzUIrcJlETM4ABSm7PDXmO-FUmvmf25TXUmqtiHj1pGqIcgRTjpw0kf_uvDUa-_ATyoUPY</recordid><startdate>20190531</startdate><enddate>20190531</enddate><creator>Kurnosov, V. B.</creator><creator>Sakharov, B. A.</creator><creator>Geptner, A. R.</creator><creator>Konovalov, Yu. I.</creator><creator>Goncharov, E. O.</creator><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20190531</creationdate><title>Clay minerals in sediments from contact zones with basalt sills</title><author>Kurnosov, V. B. ; Sakharov, B. A. ; Geptner, A. R. ; Konovalov, Yu. I. ; Goncharov, E. O.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c977-c171d27e88ba9748b9c9ac8b1447e5b3d49130d5ca21eeda8aac5dd8ef3ed60c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kurnosov, V. B.</creatorcontrib><creatorcontrib>Sakharov, B. A.</creatorcontrib><creatorcontrib>Geptner, A. R.</creatorcontrib><creatorcontrib>Konovalov, Yu. I.</creatorcontrib><creatorcontrib>Goncharov, E. O.</creatorcontrib><collection>CrossRef</collection><jtitle>Литология и полезные ископаемые</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kurnosov, V. B.</au><au>Sakharov, B. A.</au><au>Geptner, A. R.</au><au>Konovalov, Yu. I.</au><au>Goncharov, E. O.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Clay minerals in sediments from contact zones with basalt sills</atitle><jtitle>Литология и полезные ископаемые</jtitle><date>2019-05-31</date><risdate>2019</risdate><issue>3</issue><spage>234</spage><epage>247</epage><pages>234-247</pages><issn>0024-497X</issn><abstract>Clay minerals (fraction &lt;0.001 mm) of Upper Pleistocene clayey-sandy-silty sediments recovered by DSDP Holes 481 and 481A in the Northern Trough, Guaymas Basin, Gulf of California, were studied by X-ray based on the modeling of diffraction patterns and their comparison with experimental diffractograms. Terrigenous clay minerals are represented mainly by dioctahedral micaceous varieties (mixed-layer disordered illite-smectites, illite) with the chlorite admixture and by kaolinite in the upper section of unaltered sediments. Intrusion of hot basalt sills (total thickness of the complex is about 27 m) provoked alterations in the phase composition of clay minerals in sediments (7.5 m thick) overlying the sill complex. These sediments include newly formed triooctahedral layered silicates (mixed-layer chlorite-smectites, smectite). Sediments inside the sill complex include trioctahedral mixed-layer mica-smtctite-vermiculite or trioctahedral smectite. The trioctahedral mixed-layer chlorite-smectite coexisting with smectite was found in a single sample of the same complex.</abstract><doi>10.31857/S0024-497X20193234-247</doi><tpages>14</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0024-497X
ispartof Литология и полезные ископаемые, 2019-05 (3), p.234-247
issn 0024-497X
language eng
recordid cdi_crossref_primary_10_31857_S0024_497X20193234_247
source Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals
title Clay minerals in sediments from contact zones with basalt sills
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-17T09%3A55%3A33IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-crossref&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Clay%20minerals%20in%20sediments%20from%20contact%20zones%20with%20basalt%20sills&rft.jtitle=%D0%9B%D0%B8%D1%82%D0%BE%D0%BB%D0%BE%D0%B3%D0%B8%D1%8F%20%D0%B8%20%D0%BF%D0%BE%D0%BB%D0%B5%D0%B7%D0%BD%D1%8B%D0%B5%20%D0%B8%D1%81%D0%BA%D0%BE%D0%BF%D0%B0%D0%B5%D0%BC%D1%8B%D0%B5&rft.au=Kurnosov,%20V.%20B.&rft.date=2019-05-31&rft.issue=3&rft.spage=234&rft.epage=247&rft.pages=234-247&rft.issn=0024-497X&rft_id=info:doi/10.31857/S0024-497X20193234-247&rft_dat=%3Ccrossref%3E10_31857_S0024_497X20193234_247%3C/crossref%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true