Smectite-bearing clays of the Middle Eocene Kievskaya Formation in the Russian Plate and their genesis
The component composition and specific features of the structure of smectite-bearing clays in the Middle Eocene Kievskaya Formation of the Russian Plate were studied by the scanning electron microscopic, X-ray phase analysis, and complete chemical analysis methods. The clays are characterized by met...
Gespeichert in:
Veröffentlicht in: | Lithology and Mineral Resources 2012-03, Vol.47 (2), p.129-137 |
---|---|
Hauptverfasser: | , , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 137 |
---|---|
container_issue | 2 |
container_start_page | 129 |
container_title | Lithology and Mineral Resources |
container_volume | 47 |
creator | Zorina, S. O. Afanas’eva, N. I. Grevtsev, V. A. Naumkina, N. I. Mikhailov, A. A. |
description | The component composition and specific features of the structure of smectite-bearing clays in the Middle Eocene Kievskaya Formation of the Russian Plate were studied by the scanning electron microscopic, X-ray phase analysis, and complete chemical analysis methods. The clays are characterized by metastable (unstable) state of material expressed as abundance of the semidissolved clasts of felsic volcanic ashes and radiolarian skeletons, as well as colloidal segregations of siliceous, aluminosiliceous (Al-Si) and ferroaluminosiliceous (Fe-Al-Si) gel-type materials and newly formed smectite. Three stages of the diagenetic alteration of Middle Eocene dacite ashes are identified. Mechanism of the further transformation of rocks into smectite clays with siliceous nodules is proposed. The viewpoint suggesting the volcanosedimentary origin of clays of the Kievskaya Formation is confirmed. Sources of the pyroclastic material (suppliers of material for clays) in the Kievskaya Formation could be related to active explosions in the Caucasian volcanic arc in the Middle Eocene. |
doi_str_mv | 10.1134/S0024490212020071 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1022563314</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1022563314</sourcerecordid><originalsourceid>FETCH-LOGICAL-a371t-d242334f1c11b9fe25cadb3f99d4bbf243bf28b175d65caa2b2682fa8475fb3f3</originalsourceid><addsrcrecordid>eNp1kF9LwzAUxYMoOKcfwLfgky_V5Cbrn0cZm4oTxelzSdubmdk2M2mFfXtTJwiKLzfcnN85XA4hp5xdcC7k5ZIxkDJjwIEBYwnfIyMeszQSANk-GQ1yNOiH5Mj7NQt7kvER0csGy850GBWonGlXtKzV1lOrafeK9N5UVY10Zktskd4Z_PBvaqvo3LpGdca21LRf4FPvvVEtfaxVh1S11fBrHF0Fnzf-mBxoVXs8-X7H5GU-e57eRIuH69vp1SJSIuFdVIEEIaTmJedFphEmpaoKobOskkWhQYow0oInkyoOkoIC4hS0SmUy0YETY3K-y904-96j7_LG-BLrWrVoe59zBjCJheAyoGe_0LXtXRuuyzOIRThEpgHiO6h01nuHOt840yi3DUn5UHz-p_jggZ3Hb4ZC0f0E_2_6BFJ4hF4</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>926342348</pqid></control><display><type>article</type><title>Smectite-bearing clays of the Middle Eocene Kievskaya Formation in the Russian Plate and their genesis</title><source>SpringerLink Journals - AutoHoldings</source><creator>Zorina, S. O. ; Afanas’eva, N. I. ; Grevtsev, V. A. ; Naumkina, N. I. ; Mikhailov, A. A.</creator><creatorcontrib>Zorina, S. O. ; Afanas’eva, N. I. ; Grevtsev, V. A. ; Naumkina, N. I. ; Mikhailov, A. A.</creatorcontrib><description>The component composition and specific features of the structure of smectite-bearing clays in the Middle Eocene Kievskaya Formation of the Russian Plate were studied by the scanning electron microscopic, X-ray phase analysis, and complete chemical analysis methods. The clays are characterized by metastable (unstable) state of material expressed as abundance of the semidissolved clasts of felsic volcanic ashes and radiolarian skeletons, as well as colloidal segregations of siliceous, aluminosiliceous (Al-Si) and ferroaluminosiliceous (Fe-Al-Si) gel-type materials and newly formed smectite. Three stages of the diagenetic alteration of Middle Eocene dacite ashes are identified. Mechanism of the further transformation of rocks into smectite clays with siliceous nodules is proposed. The viewpoint suggesting the volcanosedimentary origin of clays of the Kievskaya Formation is confirmed. Sources of the pyroclastic material (suppliers of material for clays) in the Kievskaya Formation could be related to active explosions in the Caucasian volcanic arc in the Middle Eocene.</description><identifier>ISSN: 0024-4902</identifier><identifier>EISSN: 1608-3229</identifier><identifier>EISSN: 1573-8892</identifier><identifier>DOI: 10.1134/S0024490212020071</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Chemical analysis ; Clay ; Earth and Environmental Science ; Earth Sciences ; Eocene ; Explosions ; Geochemistry ; Geological time ; Mineral Resources ; Mineralogy ; Radiolaria ; Sedimentology</subject><ispartof>Lithology and Mineral Resources, 2012-03, Vol.47 (2), p.129-137</ispartof><rights>Pleiades Publishing, Ltd. 2012</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a371t-d242334f1c11b9fe25cadb3f99d4bbf243bf28b175d65caa2b2682fa8475fb3f3</citedby><cites>FETCH-LOGICAL-a371t-d242334f1c11b9fe25cadb3f99d4bbf243bf28b175d65caa2b2682fa8475fb3f3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S0024490212020071$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S0024490212020071$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Zorina, S. O.</creatorcontrib><creatorcontrib>Afanas’eva, N. I.</creatorcontrib><creatorcontrib>Grevtsev, V. A.</creatorcontrib><creatorcontrib>Naumkina, N. I.</creatorcontrib><creatorcontrib>Mikhailov, A. A.</creatorcontrib><title>Smectite-bearing clays of the Middle Eocene Kievskaya Formation in the Russian Plate and their genesis</title><title>Lithology and Mineral Resources</title><addtitle>Lithol Miner Resour</addtitle><description>The component composition and specific features of the structure of smectite-bearing clays in the Middle Eocene Kievskaya Formation of the Russian Plate were studied by the scanning electron microscopic, X-ray phase analysis, and complete chemical analysis methods. The clays are characterized by metastable (unstable) state of material expressed as abundance of the semidissolved clasts of felsic volcanic ashes and radiolarian skeletons, as well as colloidal segregations of siliceous, aluminosiliceous (Al-Si) and ferroaluminosiliceous (Fe-Al-Si) gel-type materials and newly formed smectite. Three stages of the diagenetic alteration of Middle Eocene dacite ashes are identified. Mechanism of the further transformation of rocks into smectite clays with siliceous nodules is proposed. The viewpoint suggesting the volcanosedimentary origin of clays of the Kievskaya Formation is confirmed. Sources of the pyroclastic material (suppliers of material for clays) in the Kievskaya Formation could be related to active explosions in the Caucasian volcanic arc in the Middle Eocene.</description><subject>Chemical analysis</subject><subject>Clay</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Eocene</subject><subject>Explosions</subject><subject>Geochemistry</subject><subject>Geological time</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Radiolaria</subject><subject>Sedimentology</subject><issn>0024-4902</issn><issn>1608-3229</issn><issn>1573-8892</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kF9LwzAUxYMoOKcfwLfgky_V5Cbrn0cZm4oTxelzSdubmdk2M2mFfXtTJwiKLzfcnN85XA4hp5xdcC7k5ZIxkDJjwIEBYwnfIyMeszQSANk-GQ1yNOiH5Mj7NQt7kvER0csGy850GBWonGlXtKzV1lOrafeK9N5UVY10Zktskd4Z_PBvaqvo3LpGdca21LRf4FPvvVEtfaxVh1S11fBrHF0Fnzf-mBxoVXs8-X7H5GU-e57eRIuH69vp1SJSIuFdVIEEIaTmJedFphEmpaoKobOskkWhQYow0oInkyoOkoIC4hS0SmUy0YETY3K-y904-96j7_LG-BLrWrVoe59zBjCJheAyoGe_0LXtXRuuyzOIRThEpgHiO6h01nuHOt840yi3DUn5UHz-p_jggZ3Hb4ZC0f0E_2_6BFJ4hF4</recordid><startdate>20120301</startdate><enddate>20120301</enddate><creator>Zorina, S. O.</creator><creator>Afanas’eva, N. I.</creator><creator>Grevtsev, V. A.</creator><creator>Naumkina, N. I.</creator><creator>Mikhailov, A. A.</creator><general>SP MAIK Nauka/Interperiodica</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7XB</scope><scope>88I</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>7TN</scope><scope>7TO</scope><scope>H94</scope><scope>H95</scope></search><sort><creationdate>20120301</creationdate><title>Smectite-bearing clays of the Middle Eocene Kievskaya Formation in the Russian Plate and their genesis</title><author>Zorina, S. O. ; Afanas’eva, N. I. ; Grevtsev, V. A. ; Naumkina, N. I. ; Mikhailov, A. A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a371t-d242334f1c11b9fe25cadb3f99d4bbf243bf28b175d65caa2b2682fa8475fb3f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Chemical analysis</topic><topic>Clay</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Eocene</topic><topic>Explosions</topic><topic>Geochemistry</topic><topic>Geological time</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Radiolaria</topic><topic>Sedimentology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zorina, S. O.</creatorcontrib><creatorcontrib>Afanas’eva, N. I.</creatorcontrib><creatorcontrib>Grevtsev, V. A.</creatorcontrib><creatorcontrib>Naumkina, N. I.</creatorcontrib><creatorcontrib>Mikhailov, A. A.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Materials Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>Oceanic Abstracts</collection><collection>Oncogenes and Growth Factors Abstracts</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><jtitle>Lithology and Mineral Resources</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zorina, S. O.</au><au>Afanas’eva, N. I.</au><au>Grevtsev, V. A.</au><au>Naumkina, N. I.</au><au>Mikhailov, A. A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Smectite-bearing clays of the Middle Eocene Kievskaya Formation in the Russian Plate and their genesis</atitle><jtitle>Lithology and Mineral Resources</jtitle><stitle>Lithol Miner Resour</stitle><date>2012-03-01</date><risdate>2012</risdate><volume>47</volume><issue>2</issue><spage>129</spage><epage>137</epage><pages>129-137</pages><issn>0024-4902</issn><eissn>1608-3229</eissn><eissn>1573-8892</eissn><abstract>The component composition and specific features of the structure of smectite-bearing clays in the Middle Eocene Kievskaya Formation of the Russian Plate were studied by the scanning electron microscopic, X-ray phase analysis, and complete chemical analysis methods. The clays are characterized by metastable (unstable) state of material expressed as abundance of the semidissolved clasts of felsic volcanic ashes and radiolarian skeletons, as well as colloidal segregations of siliceous, aluminosiliceous (Al-Si) and ferroaluminosiliceous (Fe-Al-Si) gel-type materials and newly formed smectite. Three stages of the diagenetic alteration of Middle Eocene dacite ashes are identified. Mechanism of the further transformation of rocks into smectite clays with siliceous nodules is proposed. The viewpoint suggesting the volcanosedimentary origin of clays of the Kievskaya Formation is confirmed. Sources of the pyroclastic material (suppliers of material for clays) in the Kievskaya Formation could be related to active explosions in the Caucasian volcanic arc in the Middle Eocene.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S0024490212020071</doi><tpages>9</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0024-4902 |
ispartof | Lithology and Mineral Resources, 2012-03, Vol.47 (2), p.129-137 |
issn | 0024-4902 1608-3229 1573-8892 |
language | eng |
recordid | cdi_proquest_miscellaneous_1022563314 |
source | SpringerLink Journals - AutoHoldings |
subjects | Chemical analysis Clay Earth and Environmental Science Earth Sciences Eocene Explosions Geochemistry Geological time Mineral Resources Mineralogy Radiolaria Sedimentology |
title | Smectite-bearing clays of the Middle Eocene Kievskaya Formation in the Russian Plate and their genesis |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-06T09%3A23%3A32IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Smectite-bearing%20clays%20of%20the%20Middle%20Eocene%20Kievskaya%20Formation%20in%20the%20Russian%20Plate%20and%20their%20genesis&rft.jtitle=Lithology%20and%20Mineral%20Resources&rft.au=Zorina,%20S.%20O.&rft.date=2012-03-01&rft.volume=47&rft.issue=2&rft.spage=129&rft.epage=137&rft.pages=129-137&rft.issn=0024-4902&rft.eissn=1608-3229&rft_id=info:doi/10.1134/S0024490212020071&rft_dat=%3Cproquest_cross%3E1022563314%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=926342348&rft_id=info:pmid/&rfr_iscdi=true |