A preliminary study on ore-forming environments of Xianglushan-type iron deposit and the weathering mineralization of Emeishan basalt in Guizhou Province, China
Xianglushan-type iron deposits are one of the new types of iron deposits found in the Weining Area of Western Guizhou. The iron-bearing rock system is a paleo-weathered crustal sedimentary（or accumulating） stratum between the top of the Middle-Late Permian Emeishan basalt formation and the Late Perm...
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| Veröffentlicht in: | Acta geochimica 2017-09, Vol.36 (3), p.556-565 |
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| creator | Cheng, Guofan Liu, Youping Long, Hansheng Cui, Tao Yu, Ning |
| description | Xianglushan-type iron deposits are one of the new types of iron deposits found in the Weining Area of Western Guizhou. The iron-bearing rock system is a paleo-weathered crustal sedimentary（or accumulating） stratum between the top of the Middle-Late Permian Emeishan basalt formation and the Late Permian Xuanwei formation. Iron ore is hosted in the Lower-Middle part of the rock system. In terms of the genesis of mineral deposit, this type of deposit should be a basalt paleo-weathering crustal redeposit type, very different from marine sedimentary iron deposits or continental weathering crust iron deposits. Based on field work and the analytical results of XRD Powder Diffraction, Electron Probe, Scanner Electron Microscope, etc., the geological setting of the ore-forming processes and the deposit features are illustrated in this paper. The ore-forming environment of the deposit and the Emeishan basalt weathering mineralization are also discussed in order to enhance the knowledge of the universality and diversity of mineralization of the Emeishan Large Igneous Province（ELIP）, which may be a considerable reference to further research for ELIP metallogenic theories, and geological research for iron deposits in the paleo-weathering crust areas of the Emeishan basalt,Southwestern, China. |
| doi_str_mv | 10.1007/s11631-017-0235-6 |
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The iron-bearing rock system is a paleo-weathered crustal sedimentary（or accumulating） stratum between the top of the Middle-Late Permian Emeishan basalt formation and the Late Permian Xuanwei formation. Iron ore is hosted in the Lower-Middle part of the rock system. In terms of the genesis of mineral deposit, this type of deposit should be a basalt paleo-weathering crustal redeposit type, very different from marine sedimentary iron deposits or continental weathering crust iron deposits. Based on field work and the analytical results of XRD Powder Diffraction, Electron Probe, Scanner Electron Microscope, etc., the geological setting of the ore-forming processes and the deposit features are illustrated in this paper. The ore-forming environment of the deposit and the Emeishan basalt weathering mineralization are also discussed in order to enhance the knowledge of the universality and diversity of mineralization of the Emeishan Large Igneous Province（ELIP）, which may be a considerable reference to further research for ELIP metallogenic theories, and geological research for iron deposits in the paleo-weathering crust areas of the Emeishan basalt,Southwestern, China.</description><identifier>ISSN: 2096-0956</identifier><identifier>EISSN: 2365-7499</identifier><identifier>DOI: 10.1007/s11631-017-0235-6</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Basalt ; Deposits ; Earth and Environmental Science ; Earth Sciences ; Electron probe ; Environment ; Forming ; Geochemistry ; Geology ; Iron ; Iron ores ; Mineral deposits ; Mineralization ; Original Article ; Permian ; Powder ; Provinces ; Rocks ; Volcanoes ; Weather ; Weathering ; 中国 ; 古风化壳 ; 峨眉山大火成岩省 ; 峨眉山玄武岩 ; 成矿作用 ; 成矿环境 ; 贵州省 ; 铁矿床</subject><ispartof>Acta geochimica, 2017-09, Vol.36 (3), p.556-565</ispartof><rights>Science Press, Institute of Geochemistry, CAS and Springer-Verlag GmbH Germany 2017</rights><rights>Acta Geochimica is a copyright of Springer, 2017.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a366t-a515cb20fa2479b92155ca6f0393bf4327d48cb7afe7f3c8ab0951e392b577733</citedby><cites>FETCH-LOGICAL-a366t-a515cb20fa2479b92155ca6f0393bf4327d48cb7afe7f3c8ab0951e392b577733</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/85079X/85079X.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11631-017-0235-6$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11631-017-0235-6$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,777,781,27905,27906,41469,42538,51300</link.rule.ids></links><search><creatorcontrib>Cheng, Guofan</creatorcontrib><creatorcontrib>Liu, Youping</creatorcontrib><creatorcontrib>Long, Hansheng</creatorcontrib><creatorcontrib>Cui, Tao</creatorcontrib><creatorcontrib>Yu, Ning</creatorcontrib><title>A preliminary study on ore-forming environments of Xianglushan-type iron deposit and the weathering mineralization of Emeishan basalt in Guizhou Province, China</title><title>Acta geochimica</title><addtitle>Acta Geochim</addtitle><addtitle>Chinese Journal of Geochemistry</addtitle><description>Xianglushan-type iron deposits are one of the new types of iron deposits found in the Weining Area of Western Guizhou. The iron-bearing rock system is a paleo-weathered crustal sedimentary（or accumulating） stratum between the top of the Middle-Late Permian Emeishan basalt formation and the Late Permian Xuanwei formation. Iron ore is hosted in the Lower-Middle part of the rock system. In terms of the genesis of mineral deposit, this type of deposit should be a basalt paleo-weathering crustal redeposit type, very different from marine sedimentary iron deposits or continental weathering crust iron deposits. Based on field work and the analytical results of XRD Powder Diffraction, Electron Probe, Scanner Electron Microscope, etc., the geological setting of the ore-forming processes and the deposit features are illustrated in this paper. The ore-forming environment of the deposit and the Emeishan basalt weathering mineralization are also discussed in order to enhance the knowledge of the universality and diversity of mineralization of the Emeishan Large Igneous Province（ELIP）, which may be a considerable reference to further research for ELIP metallogenic theories, and geological research for iron deposits in the paleo-weathering crust areas of the Emeishan basalt,Southwestern, China.</description><subject>Basalt</subject><subject>Deposits</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Electron probe</subject><subject>Environment</subject><subject>Forming</subject><subject>Geochemistry</subject><subject>Geology</subject><subject>Iron</subject><subject>Iron ores</subject><subject>Mineral deposits</subject><subject>Mineralization</subject><subject>Original Article</subject><subject>Permian</subject><subject>Powder</subject><subject>Provinces</subject><subject>Rocks</subject><subject>Volcanoes</subject><subject>Weather</subject><subject>Weathering</subject><subject>中国</subject><subject>古风化壳</subject><subject>峨眉山大火成岩省</subject><subject>峨眉山玄武岩</subject><subject>成矿作用</subject><subject>成矿环境</subject><subject>贵州省</subject><subject>铁矿床</subject><issn>2096-0956</issn><issn>2365-7499</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</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>eNp9UctqHDEQHIIDMY4_ILcmuVqJHiNpdTSLvQ4YnEMCuQnNrLQjMyuNJY3N-mvyqdGwxvjkUzetrqpWVdN8Ifg7wVj-yIQIRhAmEmHKOBIfmlPKBEeyVeqk9lgJhBUXn5rznO8xxmQlRNuuTpt_lzAlO_q9DyYdIJd5e4AYICaLXEx1vAMbHn2KYW9DyRAd_PUm7MY5DyagcpgsLK-wtVPMvoAJWyiDhSdrakkLQWWxyYz-2RS_cDu42lu_4KEz2YwFfIDN7J-HOMOvFB996O0FrId61OfmozNjtucv9az5c331e32Dbu82P9eXt8gwIQoynPC-o9gZ2krVKUo4741wmCnWuZZRuW1XfSeNs9KxfmW66gexTNGOSykZO2u-HXmnFB9mm4u-j3MKVVITxRWhqsWibpHjVp9izsk6PSW_r85pgvWShT5moWsWeslCLxh6xORpccOmN8zvgL6-CA0x7B4q7lVJSCbrJ7Fi_wE33ZqN</recordid><startdate>20170901</startdate><enddate>20170901</enddate><creator>Cheng, Guofan</creator><creator>Liu, Youping</creator><creator>Long, Hansheng</creator><creator>Cui, Tao</creator><creator>Yu, Ning</creator><general>Science Press</general><general>Springer Nature B.V</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>KB.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope></search><sort><creationdate>20170901</creationdate><title>A preliminary study on ore-forming environments of Xianglushan-type iron deposit and the weathering mineralization of Emeishan basalt in Guizhou Province, China</title><author>Cheng, Guofan ; Liu, Youping ; Long, Hansheng ; Cui, Tao ; Yu, Ning</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a366t-a515cb20fa2479b92155ca6f0393bf4327d48cb7afe7f3c8ab0951e392b577733</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Basalt</topic><topic>Deposits</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Electron probe</topic><topic>Environment</topic><topic>Forming</topic><topic>Geochemistry</topic><topic>Geology</topic><topic>Iron</topic><topic>Iron ores</topic><topic>Mineral deposits</topic><topic>Mineralization</topic><topic>Original Article</topic><topic>Permian</topic><topic>Powder</topic><topic>Provinces</topic><topic>Rocks</topic><topic>Volcanoes</topic><topic>Weather</topic><topic>Weathering</topic><topic>中国</topic><topic>古风化壳</topic><topic>峨眉山大火成岩省</topic><topic>峨眉山玄武岩</topic><topic>成矿作用</topic><topic>成矿环境</topic><topic>贵州省</topic><topic>铁矿床</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cheng, Guofan</creatorcontrib><creatorcontrib>Liu, Youping</creatorcontrib><creatorcontrib>Long, Hansheng</creatorcontrib><creatorcontrib>Cui, Tao</creatorcontrib><creatorcontrib>Yu, Ning</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-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Water Resources Abstracts</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 SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Materials Science Collection</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</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>Materials Science Database</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Materials Science Collection</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Acta geochimica</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cheng, Guofan</au><au>Liu, Youping</au><au>Long, Hansheng</au><au>Cui, Tao</au><au>Yu, Ning</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A preliminary study on ore-forming environments of Xianglushan-type iron deposit and the weathering mineralization of Emeishan basalt in Guizhou Province, China</atitle><jtitle>Acta geochimica</jtitle><stitle>Acta Geochim</stitle><addtitle>Chinese Journal of Geochemistry</addtitle><date>2017-09-01</date><risdate>2017</risdate><volume>36</volume><issue>3</issue><spage>556</spage><epage>565</epage><pages>556-565</pages><issn>2096-0956</issn><eissn>2365-7499</eissn><abstract>Xianglushan-type iron deposits are one of the new types of iron deposits found in the Weining Area of Western Guizhou. The iron-bearing rock system is a paleo-weathered crustal sedimentary（or accumulating） stratum between the top of the Middle-Late Permian Emeishan basalt formation and the Late Permian Xuanwei formation. Iron ore is hosted in the Lower-Middle part of the rock system. In terms of the genesis of mineral deposit, this type of deposit should be a basalt paleo-weathering crustal redeposit type, very different from marine sedimentary iron deposits or continental weathering crust iron deposits. Based on field work and the analytical results of XRD Powder Diffraction, Electron Probe, Scanner Electron Microscope, etc., the geological setting of the ore-forming processes and the deposit features are illustrated in this paper. The ore-forming environment of the deposit and the Emeishan basalt weathering mineralization are also discussed in order to enhance the knowledge of the universality and diversity of mineralization of the Emeishan Large Igneous Province（ELIP）, which may be a considerable reference to further research for ELIP metallogenic theories, and geological research for iron deposits in the paleo-weathering crust areas of the Emeishan basalt,Southwestern, China.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s11631-017-0235-6</doi><tpages>10</tpages></addata></record> |
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| subjects | Basalt Deposits Earth and Environmental Science Earth Sciences Electron probe Environment Forming Geochemistry Geology Iron Iron ores Mineral deposits Mineralization Original Article Permian Powder Provinces Rocks Volcanoes Weather Weathering 中国 古风化壳 峨眉山大火成岩省 峨眉山玄武岩 成矿作用 成矿环境 贵州省 铁矿床 |
| title | A preliminary study on ore-forming environments of Xianglushan-type iron deposit and the weathering mineralization of Emeishan basalt in Guizhou Province, China |
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