Strontium Isotope Compositions of Hydrothermal Barite from the Yonaguni IV: Insight into Fluid/Sediment Interaction and Barite Crystallization Condition
Hydrothermal barite is a typical low-temperature mineral formed during the mixing of hydrothermal fluid and seawater. Because of its extremely low solubility, barite behaves as a close system after crystallization and preserves the geochemical fingerprint of hydrothermal fluid. In this study, the el...
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| Veröffentlicht in: | Journal of Ocean University of China 2020-04, Vol.19 (2), p.377-385 |
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| description | Hydrothermal barite is a typical low-temperature mineral formed during the mixing of hydrothermal fluid and seawater. Because of its extremely low solubility, barite behaves as a close system after crystallization and preserves the geochemical fingerprint of hydrothermal fluid. In this study, the elemental contents and Sr isotope compositions of hydrothermal barites from the Yonaguni IV were determined using electron microprobe and LA-MC-ICP-MS respectively. On these bases, the fluid/sediment interaction during the hydrothermal circulation and physicochemical condition of barite crystallization were discussed. Results show that the 87Sr/86Sr values of hydrothermal barites from the Yonaguni IV are apparently higher than those of the seawater and associated volcanic rocks, indicating the sufficient interaction between the hydrothermal fluid and overlying sediment. Monomineral Sr abundance shows large variations, reflecting the changes in barite growth rate during the fluid mixing. The mineralization condition in the Yonaguni IV was unstable. During the crystallization of barite, hydrothermal fluid and seawater mixed in varying degrees, with the proportions of hydrothermal fluid varied from 36% to 72%. The calculated crystallization temperatures range from 109 to 220°C. Sediment plays a critical role during the mineralization process in the Yonaguni IV and incorporation of sediment component into hydrothermal system was prior to barite crystallization and sulfide mineralization. |
| doi_str_mv | 10.1007/s11802-020-4021-4 |
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Because of its extremely low solubility, barite behaves as a close system after crystallization and preserves the geochemical fingerprint of hydrothermal fluid. In this study, the elemental contents and Sr isotope compositions of hydrothermal barites from the Yonaguni IV were determined using electron microprobe and LA-MC-ICP-MS respectively. On these bases, the fluid/sediment interaction during the hydrothermal circulation and physicochemical condition of barite crystallization were discussed. Results show that the 87Sr/86Sr values of hydrothermal barites from the Yonaguni IV are apparently higher than those of the seawater and associated volcanic rocks, indicating the sufficient interaction between the hydrothermal fluid and overlying sediment. Monomineral Sr abundance shows large variations, reflecting the changes in barite growth rate during the fluid mixing. The mineralization condition in the Yonaguni IV was unstable. During the crystallization of barite, hydrothermal fluid and seawater mixed in varying degrees, with the proportions of hydrothermal fluid varied from 36% to 72%. The calculated crystallization temperatures range from 109 to 220°C. Sediment plays a critical role during the mineralization process in the Yonaguni IV and incorporation of sediment component into hydrothermal system was prior to barite crystallization and sulfide mineralization.</description><identifier>ISSN: 1672-5182</identifier><identifier>EISSN: 1993-5021</identifier><identifier>EISSN: 1672-5174</identifier><identifier>DOI: 10.1007/s11802-020-4021-4</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Barite ; Chemical fingerprinting ; Composition ; Crystallization ; Earth and Environmental Science ; Earth Sciences ; Electron microprobe ; Electron probes ; Growth rate ; Hydrothermal systems ; Isotopes ; Low temperature ; Meteorology ; Mineralization ; Oceanography ; Seawater ; Sediment ; Sediments ; Strontium ; Strontium 87 ; Strontium isotopes ; Sulfides ; Sulphides ; Volcanic rocks</subject><ispartof>Journal of Ocean University of China, 2020-04, Vol.19 (2), p.377-385</ispartof><rights>Ocean University of China, Science Press and Springer-Verlag GmbH Germany 2020</rights><rights>2020© Ocean University of China, Science Press and Springer-Verlag GmbH Germany 2020</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c352t-b5e59221f7e9412d3471e7176be1b4aa67f6052864821e68f4b5fa1befda6ada3</citedby><cites>FETCH-LOGICAL-c352t-b5e59221f7e9412d3471e7176be1b4aa67f6052864821e68f4b5fa1befda6ada3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/qdhydxxb-e/qdhydxxb-e.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11802-020-4021-4$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11802-020-4021-4$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids></links><search><creatorcontrib>Zhang, Xia</creatorcontrib><creatorcontrib>Zhai, Shikui</creatorcontrib><creatorcontrib>Yu, Zenghui</creatorcontrib><title>Strontium Isotope Compositions of Hydrothermal Barite from the Yonaguni IV: Insight into Fluid/Sediment Interaction and Barite Crystallization Condition</title><title>Journal of Ocean University of China</title><addtitle>J. Ocean Univ. China</addtitle><description>Hydrothermal barite is a typical low-temperature mineral formed during the mixing of hydrothermal fluid and seawater. Because of its extremely low solubility, barite behaves as a close system after crystallization and preserves the geochemical fingerprint of hydrothermal fluid. In this study, the elemental contents and Sr isotope compositions of hydrothermal barites from the Yonaguni IV were determined using electron microprobe and LA-MC-ICP-MS respectively. On these bases, the fluid/sediment interaction during the hydrothermal circulation and physicochemical condition of barite crystallization were discussed. Results show that the 87Sr/86Sr values of hydrothermal barites from the Yonaguni IV are apparently higher than those of the seawater and associated volcanic rocks, indicating the sufficient interaction between the hydrothermal fluid and overlying sediment. Monomineral Sr abundance shows large variations, reflecting the changes in barite growth rate during the fluid mixing. The mineralization condition in the Yonaguni IV was unstable. During the crystallization of barite, hydrothermal fluid and seawater mixed in varying degrees, with the proportions of hydrothermal fluid varied from 36% to 72%. The calculated crystallization temperatures range from 109 to 220°C. Sediment plays a critical role during the mineralization process in the Yonaguni IV and incorporation of sediment component into hydrothermal system was prior to barite crystallization and sulfide mineralization.</description><subject>Barite</subject><subject>Chemical fingerprinting</subject><subject>Composition</subject><subject>Crystallization</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Electron microprobe</subject><subject>Electron probes</subject><subject>Growth rate</subject><subject>Hydrothermal systems</subject><subject>Isotopes</subject><subject>Low temperature</subject><subject>Meteorology</subject><subject>Mineralization</subject><subject>Oceanography</subject><subject>Seawater</subject><subject>Sediment</subject><subject>Sediments</subject><subject>Strontium</subject><subject>Strontium 87</subject><subject>Strontium isotopes</subject><subject>Sulfides</subject><subject>Sulphides</subject><subject>Volcanic rocks</subject><issn>1672-5182</issn><issn>1993-5021</issn><issn>1672-5174</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp1kcFu1DAQhiMEEqXwANwscUShHseOE24QUbpSJQ4FJE7WZG3vukrsre2ILk_C4-JtQD0hWRp75vv_kfxX1Wug74BSeZEAOspqymjNKYOaP6nOoO-bWpTX03JvJasFdOx59SKlW0pFI1p5Vv2-yTH47JaZbFLI4WDIEOZDSC674BMJllwddQx5b-KME_mI0WVDbAwzKT3yI3jcLd6Rzff3ZOOT2-0zcT4HcjktTl_cGO1m43OZZRNxe3Il6PU_oyEeU8Zpcr_wYTQErx9Wv6yeWZySefW3nlffLj99Ha7q6y-fN8OH63rbCJbrURjRMwZWmp4D0w2XYCTIdjQwcsRW2pYK1rW8Y2DazvJRWITRWI0tamzOq7er70_0Fv1O3YYl-rJR3en9Ud_fj8qw8q3lQFPoNyt9iOFuMSk_4qzhXAgOsi8UrNQ2hpSiseoQ3YzxqICqU1xqjUsVU3WKS_GiYasmFdbvTHx0_r_oDzDTmpQ</recordid><startdate>20200401</startdate><enddate>20200401</enddate><creator>Zhang, Xia</creator><creator>Zhai, Shikui</creator><creator>Yu, Zenghui</creator><general>Science Press</general><general>Springer Nature B.V</general><general>Key Laboratory of Submarine Geosciences and Prospecting Techniques, Ministry of Education, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7T7</scope><scope>7TN</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope><scope>P64</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20200401</creationdate><title>Strontium Isotope Compositions of Hydrothermal Barite from the Yonaguni IV: Insight into Fluid/Sediment Interaction and Barite Crystallization Condition</title><author>Zhang, Xia ; Zhai, Shikui ; Yu, Zenghui</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c352t-b5e59221f7e9412d3471e7176be1b4aa67f6052864821e68f4b5fa1befda6ada3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Barite</topic><topic>Chemical fingerprinting</topic><topic>Composition</topic><topic>Crystallization</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Electron microprobe</topic><topic>Electron probes</topic><topic>Growth rate</topic><topic>Hydrothermal systems</topic><topic>Isotopes</topic><topic>Low temperature</topic><topic>Meteorology</topic><topic>Mineralization</topic><topic>Oceanography</topic><topic>Seawater</topic><topic>Sediment</topic><topic>Sediments</topic><topic>Strontium</topic><topic>Strontium 87</topic><topic>Strontium isotopes</topic><topic>Sulfides</topic><topic>Sulphides</topic><topic>Volcanic rocks</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhang, Xia</creatorcontrib><creatorcontrib>Zhai, Shikui</creatorcontrib><creatorcontrib>Yu, Zenghui</creatorcontrib><collection>CrossRef</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Journal of Ocean University of China</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhang, Xia</au><au>Zhai, Shikui</au><au>Yu, Zenghui</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Strontium Isotope Compositions of Hydrothermal Barite from the Yonaguni IV: Insight into Fluid/Sediment Interaction and Barite Crystallization Condition</atitle><jtitle>Journal of Ocean University of China</jtitle><stitle>J. Ocean Univ. China</stitle><date>2020-04-01</date><risdate>2020</risdate><volume>19</volume><issue>2</issue><spage>377</spage><epage>385</epage><pages>377-385</pages><issn>1672-5182</issn><eissn>1993-5021</eissn><eissn>1672-5174</eissn><abstract>Hydrothermal barite is a typical low-temperature mineral formed during the mixing of hydrothermal fluid and seawater. Because of its extremely low solubility, barite behaves as a close system after crystallization and preserves the geochemical fingerprint of hydrothermal fluid. In this study, the elemental contents and Sr isotope compositions of hydrothermal barites from the Yonaguni IV were determined using electron microprobe and LA-MC-ICP-MS respectively. On these bases, the fluid/sediment interaction during the hydrothermal circulation and physicochemical condition of barite crystallization were discussed. Results show that the 87Sr/86Sr values of hydrothermal barites from the Yonaguni IV are apparently higher than those of the seawater and associated volcanic rocks, indicating the sufficient interaction between the hydrothermal fluid and overlying sediment. Monomineral Sr abundance shows large variations, reflecting the changes in barite growth rate during the fluid mixing. The mineralization condition in the Yonaguni IV was unstable. During the crystallization of barite, hydrothermal fluid and seawater mixed in varying degrees, with the proportions of hydrothermal fluid varied from 36% to 72%. The calculated crystallization temperatures range from 109 to 220°C. Sediment plays a critical role during the mineralization process in the Yonaguni IV and incorporation of sediment component into hydrothermal system was prior to barite crystallization and sulfide mineralization.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s11802-020-4021-4</doi><tpages>9</tpages></addata></record> |
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| source | Springer Nature - Complete Springer Journals; Alma/SFX Local Collection |
| subjects | Barite Chemical fingerprinting Composition Crystallization Earth and Environmental Science Earth Sciences Electron microprobe Electron probes Growth rate Hydrothermal systems Isotopes Low temperature Meteorology Mineralization Oceanography Seawater Sediment Sediments Strontium Strontium 87 Strontium isotopes Sulfides Sulphides Volcanic rocks |
| title | Strontium Isotope Compositions of Hydrothermal Barite from the Yonaguni IV: Insight into Fluid/Sediment Interaction and Barite Crystallization Condition |
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