Mineralogical Characterisation of the Sedimentary Phosphate Deposit of Tobene (Western Senegal)
The Tobrne panel is the third of the Ta'fba phosphate deposit. This mineralogical study contributes to the improved knowledge of the various facies that comprise the phosphate series of Tobrne. Based on X-ray diffraction results, the Tobrne panel yielded minerals that are primarily divided into four...
Gespeichert in:
Veröffentlicht in: | 船舶与海洋工程:英文版 2016, Vol.6 (4), p.226-240 |
---|---|
1. Verfasser: | |
Format: | Artikel |
Sprache: | eng |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 240 |
---|---|
container_issue | 4 |
container_start_page | 226 |
container_title | 船舶与海洋工程:英文版 |
container_volume | 6 |
creator | Moustapha Diagne Mamadou Fall Mouhamadou Bachir Diouf Ndeye Penda Dione El Hadji MansourSamb |
description | The Tobrne panel is the third of the Ta'fba phosphate deposit. This mineralogical study contributes to the improved knowledge of the various facies that comprise the phosphate series of Tobrne. Based on X-ray diffraction results, the Tobrne panel yielded minerals that are primarily divided into four groups: minerals of the original phosphate phase: apatite, fluorapatite; carbonate minerals: calcite and dolomite; clay minerals: palygorskite, smectite, kaolinite and illite; minerals of altered facies: alteration minerals (analcime, millisite, crandallite and wavellite) and ferruginous minerals (goethite and gibbsite). This succession of mineralogical associations reflects a polyphase alteration leading to a vertical and lateral facies sequence. This alteration intensifies the phosphate series upward and laterally from West to East. |
format | Article |
fullrecord | <record><control><sourceid>chongqing</sourceid><recordid>TN_cdi_chongqing_primary_669471317</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>669471317</cqvip_id><sourcerecordid>669471317</sourcerecordid><originalsourceid>FETCH-chongqing_primary_6694713173</originalsourceid><addsrcrecordid>eNqNjEEKwjAURIMoKOodgvuCbW1r1lVxIwgWXMq3_iaRmNQkG2-gd-qdegUriGtnM7N4b3pkFIUJC5LlMuv_dsaGZOrcdd4lSVjE5iNS7qRGC8pwWYKiuQALpUcrHXhpNDUV9QLpAS_yhtqDfdC9MK4W4JGusDZO-g9UmDNqpG3zPKLrfN0pGjmotnlNyKAC5XD67TGZbdZFvg1KYTS_S81PtZW37vuUpmyRhXGYxX9Bbx8PSdY</addsrcrecordid><sourcetype>Publisher</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Mineralogical Characterisation of the Sedimentary Phosphate Deposit of Tobene (Western Senegal)</title><source>EZB-FREE-00999 freely available EZB journals</source><creator>Moustapha Diagne Mamadou Fall Mouhamadou Bachir Diouf Ndeye Penda Dione El Hadji MansourSamb</creator><creatorcontrib>Moustapha Diagne Mamadou Fall Mouhamadou Bachir Diouf Ndeye Penda Dione El Hadji MansourSamb</creatorcontrib><description>The Tobrne panel is the third of the Ta'fba phosphate deposit. This mineralogical study contributes to the improved knowledge of the various facies that comprise the phosphate series of Tobrne. Based on X-ray diffraction results, the Tobrne panel yielded minerals that are primarily divided into four groups: minerals of the original phosphate phase: apatite, fluorapatite; carbonate minerals: calcite and dolomite; clay minerals: palygorskite, smectite, kaolinite and illite; minerals of altered facies: alteration minerals (analcime, millisite, crandallite and wavellite) and ferruginous minerals (goethite and gibbsite). This succession of mineralogical associations reflects a polyphase alteration leading to a vertical and lateral facies sequence. This alteration intensifies the phosphate series upward and laterally from West to East.</description><identifier>ISSN: 2159-5879</identifier><identifier>EISSN: 2159-5887</identifier><language>eng</language><ispartof>船舶与海洋工程:英文版, 2016, Vol.6 (4), p.226-240</ispartof><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/71223X/71223X.jpg</thumbnail><link.rule.ids>314,776,780,4010</link.rule.ids></links><search><creatorcontrib>Moustapha Diagne Mamadou Fall Mouhamadou Bachir Diouf Ndeye Penda Dione El Hadji MansourSamb</creatorcontrib><title>Mineralogical Characterisation of the Sedimentary Phosphate Deposit of Tobene (Western Senegal)</title><title>船舶与海洋工程:英文版</title><addtitle>Journal of Shipping and Ocean Engineering</addtitle><description>The Tobrne panel is the third of the Ta'fba phosphate deposit. This mineralogical study contributes to the improved knowledge of the various facies that comprise the phosphate series of Tobrne. Based on X-ray diffraction results, the Tobrne panel yielded minerals that are primarily divided into four groups: minerals of the original phosphate phase: apatite, fluorapatite; carbonate minerals: calcite and dolomite; clay minerals: palygorskite, smectite, kaolinite and illite; minerals of altered facies: alteration minerals (analcime, millisite, crandallite and wavellite) and ferruginous minerals (goethite and gibbsite). This succession of mineralogical associations reflects a polyphase alteration leading to a vertical and lateral facies sequence. This alteration intensifies the phosphate series upward and laterally from West to East.</description><issn>2159-5879</issn><issn>2159-5887</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNqNjEEKwjAURIMoKOodgvuCbW1r1lVxIwgWXMq3_iaRmNQkG2-gd-qdegUriGtnM7N4b3pkFIUJC5LlMuv_dsaGZOrcdd4lSVjE5iNS7qRGC8pwWYKiuQALpUcrHXhpNDUV9QLpAS_yhtqDfdC9MK4W4JGusDZO-g9UmDNqpG3zPKLrfN0pGjmotnlNyKAC5XD67TGZbdZFvg1KYTS_S81PtZW37vuUpmyRhXGYxX9Bbx8PSdY</recordid><startdate>2016</startdate><enddate>2016</enddate><creator>Moustapha Diagne Mamadou Fall Mouhamadou Bachir Diouf Ndeye Penda Dione El Hadji MansourSamb</creator><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W92</scope><scope>~WA</scope></search><sort><creationdate>2016</creationdate><title>Mineralogical Characterisation of the Sedimentary Phosphate Deposit of Tobene (Western Senegal)</title><author>Moustapha Diagne Mamadou Fall Mouhamadou Bachir Diouf Ndeye Penda Dione El Hadji MansourSamb</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-chongqing_primary_6694713173</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><toplevel>online_resources</toplevel><creatorcontrib>Moustapha Diagne Mamadou Fall Mouhamadou Bachir Diouf Ndeye Penda Dione El Hadji MansourSamb</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-工程技术</collection><collection>中文科技期刊数据库- 镜像站点</collection><jtitle>船舶与海洋工程:英文版</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Moustapha Diagne Mamadou Fall Mouhamadou Bachir Diouf Ndeye Penda Dione El Hadji MansourSamb</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Mineralogical Characterisation of the Sedimentary Phosphate Deposit of Tobene (Western Senegal)</atitle><jtitle>船舶与海洋工程:英文版</jtitle><addtitle>Journal of Shipping and Ocean Engineering</addtitle><date>2016</date><risdate>2016</risdate><volume>6</volume><issue>4</issue><spage>226</spage><epage>240</epage><pages>226-240</pages><issn>2159-5879</issn><eissn>2159-5887</eissn><abstract>The Tobrne panel is the third of the Ta'fba phosphate deposit. This mineralogical study contributes to the improved knowledge of the various facies that comprise the phosphate series of Tobrne. Based on X-ray diffraction results, the Tobrne panel yielded minerals that are primarily divided into four groups: minerals of the original phosphate phase: apatite, fluorapatite; carbonate minerals: calcite and dolomite; clay minerals: palygorskite, smectite, kaolinite and illite; minerals of altered facies: alteration minerals (analcime, millisite, crandallite and wavellite) and ferruginous minerals (goethite and gibbsite). This succession of mineralogical associations reflects a polyphase alteration leading to a vertical and lateral facies sequence. This alteration intensifies the phosphate series upward and laterally from West to East.</abstract></addata></record> |
fulltext | fulltext |
identifier | ISSN: 2159-5879 |
ispartof | 船舶与海洋工程:英文版, 2016, Vol.6 (4), p.226-240 |
issn | 2159-5879 2159-5887 |
language | eng |
recordid | cdi_chongqing_primary_669471317 |
source | EZB-FREE-00999 freely available EZB journals |
title | Mineralogical Characterisation of the Sedimentary Phosphate Deposit of Tobene (Western Senegal) |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-10T10%3A54%3A40IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-chongqing&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Mineralogical%20Characterisation%20of%20the%20Sedimentary%20Phosphate%20Deposit%20of%20Tobene%20%EF%BC%88Western%20Senegal%EF%BC%89&rft.jtitle=%E8%88%B9%E8%88%B6%E4%B8%8E%E6%B5%B7%E6%B4%8B%E5%B7%A5%E7%A8%8B%EF%BC%9A%E8%8B%B1%E6%96%87%E7%89%88&rft.au=Moustapha%20Diagne%20Mamadou%20Fall%20Mouhamadou%20Bachir%20Diouf%20Ndeye%20Penda%20Dione%20El%20Hadji%20MansourSamb&rft.date=2016&rft.volume=6&rft.issue=4&rft.spage=226&rft.epage=240&rft.pages=226-240&rft.issn=2159-5879&rft.eissn=2159-5887&rft_id=info:doi/&rft_dat=%3Cchongqing%3E669471317%3C/chongqing%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_cqvip_id=669471317&rfr_iscdi=true |