Ferromanganese crusts from the Sea of Okhotsk

New data on the microstructures and the mineral and chemical compositions of ferromanganese crusts obtained from the western slope of the Kuril Island Arc in the Sea of Okhotsk during cruises of the R/V Vulkanolog are discussed. The study of the crusts using analytical electron microscopy methods re...

Full description

Saved in:
Bibliographic Details
Published in:Oceanology (Washington. 1965) 2012-02, Vol.52 (1), p.88-100
Main Authors: Baturin, G. N., Dubinchuk, V. T., Rashidov, V. A.
Format: Article
Language:English
Subjects:
Analytical chemistry
Chemical analysis
Earth and Environmental Science
Earth Sciences
Island arcs
Manganese
Marine
Marine Geology
Montmorillonite
Morphology
Oceanography
Rare earth elements
Seismology
Trace elements
Volcanology
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c347t-e9374d031abc777734ac8d67f74bbcd5c337a10b9106fe8697e4a4004ccf189a3
cites cdi_FETCH-LOGICAL-c347t-e9374d031abc777734ac8d67f74bbcd5c337a10b9106fe8697e4a4004ccf189a3
container_end_page 100
container_issue 1
container_start_page 88
container_title Oceanology (Washington. 1965)
container_volume 52
creator Baturin, G. N.
Dubinchuk, V. T.
Rashidov, V. A.
description New data on the microstructures and the mineral and chemical compositions of ferromanganese crusts obtained from the western slope of the Kuril Island Arc in the Sea of Okhotsk during cruises of the R/V Vulkanolog are discussed. The study of the crusts using analytical electron microscopy methods revealed that their manganese phase is represented by vernadite, Fe-vernadite, todorokite, asbolane, and asbolane-buserite, while the iron phase consists of hematite, hydrohematite, ferroxyhite, and magnetite. The assemblage of lithic minerals includes apatite, quartz, epidote, and montmorillonite. According to the chemical analysis, most of the crusts contain a significant share of volcanogenic and hydrothermal material, which is evident from the elevated values of the Mn and Ti modules, the low concentrations of some trace elements, and the positive Eu anomaly in the rare earth elements composition.
doi_str_mv 10.1134/S0001437012010031
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_954650969</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>954650969</sourcerecordid><originalsourceid>FETCH-LOGICAL-c347t-e9374d031abc777734ac8d67f74bbcd5c337a10b9106fe8697e4a4004ccf189a3</originalsourceid><addsrcrecordid>eNp1kE1LxDAQhoMouK7-AG_Fi6fqTJM2zVEWv2BhD6vnkGaT_W7WTHvw35uygqA4l4F5n_edYRi7RrhD5OJ-DgAouAQsAAE4nrARlhzzuoT6lI0GOR_0c3ZBtBkIoeoRy59cjGFv2qVpHbnMxp46ynyaZd3KZXNnsuCz2XYVOtpesjNvduSuvvuYvT89vk1e8uns-XXyMM0tF7LLneJSLNIK01iZigtj60UlvRRNYxel5VwahEYhVN7VlZJOGAEgrPVYK8PH7PaYe4jho3fU6f2arNvt0pGhJ61KUZWgKpXIm1_kJvSxTcdpVXCuiqKEBOERsjEQRef1Ia73Jn5qBD28T_95X_IURw8ltl26-BP8v-kLSIBuuA</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>923392250</pqid></control><display><type>article</type><title>Ferromanganese crusts from the Sea of Okhotsk</title><source>Springer Nature</source><creator>Baturin, G. N. ; Dubinchuk, V. T. ; Rashidov, V. A.</creator><creatorcontrib>Baturin, G. N. ; Dubinchuk, V. T. ; Rashidov, V. A.</creatorcontrib><description>New data on the microstructures and the mineral and chemical compositions of ferromanganese crusts obtained from the western slope of the Kuril Island Arc in the Sea of Okhotsk during cruises of the R/V Vulkanolog are discussed. The study of the crusts using analytical electron microscopy methods revealed that their manganese phase is represented by vernadite, Fe-vernadite, todorokite, asbolane, and asbolane-buserite, while the iron phase consists of hematite, hydrohematite, ferroxyhite, and magnetite. The assemblage of lithic minerals includes apatite, quartz, epidote, and montmorillonite. According to the chemical analysis, most of the crusts contain a significant share of volcanogenic and hydrothermal material, which is evident from the elevated values of the Mn and Ti modules, the low concentrations of some trace elements, and the positive Eu anomaly in the rare earth elements composition.</description><identifier>ISSN: 0001-4370</identifier><identifier>EISSN: 1531-8508</identifier><identifier>DOI: 10.1134/S0001437012010031</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Analytical chemistry ; Chemical analysis ; Earth and Environmental Science ; Earth Sciences ; Island arcs ; Manganese ; Marine ; Marine Geology ; Montmorillonite ; Morphology ; Oceanography ; Rare earth elements ; Seismology ; Trace elements ; Volcanology</subject><ispartof>Oceanology (Washington. 1965), 2012-02, Vol.52 (1), p.88-100</ispartof><rights>Pleiades Publishing, Ltd. 2012</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c347t-e9374d031abc777734ac8d67f74bbcd5c337a10b9106fe8697e4a4004ccf189a3</citedby><cites>FETCH-LOGICAL-c347t-e9374d031abc777734ac8d67f74bbcd5c337a10b9106fe8697e4a4004ccf189a3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27903,27904</link.rule.ids></links><search><creatorcontrib>Baturin, G. N.</creatorcontrib><creatorcontrib>Dubinchuk, V. T.</creatorcontrib><creatorcontrib>Rashidov, V. A.</creatorcontrib><title>Ferromanganese crusts from the Sea of Okhotsk</title><title>Oceanology (Washington. 1965)</title><addtitle>Oceanology</addtitle><description>New data on the microstructures and the mineral and chemical compositions of ferromanganese crusts obtained from the western slope of the Kuril Island Arc in the Sea of Okhotsk during cruises of the R/V Vulkanolog are discussed. The study of the crusts using analytical electron microscopy methods revealed that their manganese phase is represented by vernadite, Fe-vernadite, todorokite, asbolane, and asbolane-buserite, while the iron phase consists of hematite, hydrohematite, ferroxyhite, and magnetite. The assemblage of lithic minerals includes apatite, quartz, epidote, and montmorillonite. According to the chemical analysis, most of the crusts contain a significant share of volcanogenic and hydrothermal material, which is evident from the elevated values of the Mn and Ti modules, the low concentrations of some trace elements, and the positive Eu anomaly in the rare earth elements composition.</description><subject>Analytical chemistry</subject><subject>Chemical analysis</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Island arcs</subject><subject>Manganese</subject><subject>Marine</subject><subject>Marine Geology</subject><subject>Montmorillonite</subject><subject>Morphology</subject><subject>Oceanography</subject><subject>Rare earth elements</subject><subject>Seismology</subject><subject>Trace elements</subject><subject>Volcanology</subject><issn>0001-4370</issn><issn>1531-8508</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNp1kE1LxDAQhoMouK7-AG_Fi6fqTJM2zVEWv2BhD6vnkGaT_W7WTHvw35uygqA4l4F5n_edYRi7RrhD5OJ-DgAouAQsAAE4nrARlhzzuoT6lI0GOR_0c3ZBtBkIoeoRy59cjGFv2qVpHbnMxp46ynyaZd3KZXNnsuCz2XYVOtpesjNvduSuvvuYvT89vk1e8uns-XXyMM0tF7LLneJSLNIK01iZigtj60UlvRRNYxel5VwahEYhVN7VlZJOGAEgrPVYK8PH7PaYe4jho3fU6f2arNvt0pGhJ61KUZWgKpXIm1_kJvSxTcdpVXCuiqKEBOERsjEQRef1Ia73Jn5qBD28T_95X_IURw8ltl26-BP8v-kLSIBuuA</recordid><startdate>20120201</startdate><enddate>20120201</enddate><creator>Baturin, G. N.</creator><creator>Dubinchuk, V. T.</creator><creator>Rashidov, V. A.</creator><general>SP MAIK Nauka/Interperiodica</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope></search><sort><creationdate>20120201</creationdate><title>Ferromanganese crusts from the Sea of Okhotsk</title><author>Baturin, G. N. ; Dubinchuk, V. T. ; Rashidov, V. A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c347t-e9374d031abc777734ac8d67f74bbcd5c337a10b9106fe8697e4a4004ccf189a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Analytical chemistry</topic><topic>Chemical analysis</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Island arcs</topic><topic>Manganese</topic><topic>Marine</topic><topic>Marine Geology</topic><topic>Montmorillonite</topic><topic>Morphology</topic><topic>Oceanography</topic><topic>Rare earth elements</topic><topic>Seismology</topic><topic>Trace elements</topic><topic>Volcanology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Baturin, G. N.</creatorcontrib><creatorcontrib>Dubinchuk, V. T.</creatorcontrib><creatorcontrib>Rashidov, V. A.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Science Journals</collection><collection>Environmental Science Database</collection><collection>ProQuest Earth, Atmospheric &amp; 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>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Oceanology (Washington. 1965)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Baturin, G. N.</au><au>Dubinchuk, V. T.</au><au>Rashidov, V. A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Ferromanganese crusts from the Sea of Okhotsk</atitle><jtitle>Oceanology (Washington. 1965)</jtitle><stitle>Oceanology</stitle><date>2012-02-01</date><risdate>2012</risdate><volume>52</volume><issue>1</issue><spage>88</spage><epage>100</epage><pages>88-100</pages><issn>0001-4370</issn><eissn>1531-8508</eissn><abstract>New data on the microstructures and the mineral and chemical compositions of ferromanganese crusts obtained from the western slope of the Kuril Island Arc in the Sea of Okhotsk during cruises of the R/V Vulkanolog are discussed. The study of the crusts using analytical electron microscopy methods revealed that their manganese phase is represented by vernadite, Fe-vernadite, todorokite, asbolane, and asbolane-buserite, while the iron phase consists of hematite, hydrohematite, ferroxyhite, and magnetite. The assemblage of lithic minerals includes apatite, quartz, epidote, and montmorillonite. According to the chemical analysis, most of the crusts contain a significant share of volcanogenic and hydrothermal material, which is evident from the elevated values of the Mn and Ti modules, the low concentrations of some trace elements, and the positive Eu anomaly in the rare earth elements composition.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S0001437012010031</doi><tpages>13</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0001-4370
ispartof Oceanology (Washington. 1965), 2012-02, Vol.52 (1), p.88-100
issn 0001-4370
1531-8508
language eng
recordid cdi_proquest_miscellaneous_954650969
source Springer Nature
subjects Analytical chemistry
Chemical analysis
Earth and Environmental Science
Earth Sciences
Island arcs
Manganese
Marine
Marine Geology
Montmorillonite
Morphology
Oceanography
Rare earth elements
Seismology
Trace elements
Volcanology
title Ferromanganese crusts from the Sea of Okhotsk
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-24T19%3A45%3A37IST&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=Ferromanganese%20crusts%20from%20the%20Sea%20of%20Okhotsk&rft.jtitle=Oceanology%20(Washington.%201965)&rft.au=Baturin,%20G.%20N.&rft.date=2012-02-01&rft.volume=52&rft.issue=1&rft.spage=88&rft.epage=100&rft.pages=88-100&rft.issn=0001-4370&rft.eissn=1531-8508&rft_id=info:doi/10.1134/S0001437012010031&rft_dat=%3Cproquest_cross%3E954650969%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c347t-e9374d031abc777734ac8d67f74bbcd5c337a10b9106fe8697e4a4004ccf189a3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=923392250&rft_id=info:pmid/&rfr_iscdi=true