The Tafak manganese deposit (Dursunbey-Balıkesir, NW Turkey): implications for the submarine hydrothermal origin of İzmir-Ankara-Erzincan Neotethyan Ocean
In Turkey, radiolarian chert-hosted Mn-oxide deposits are exposed commonly within the deep-sea pelagic sediments belonging to the ophiolitic mélange units along northern branch of the Neotethys (İzmir-Ankara-Erzincan Suture Zone) in northern Turkey. In the Tafak region (Dursunbey, Balıkesir), Mn-dep...
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| description | In Turkey, radiolarian chert-hosted Mn-oxide deposits are exposed commonly within the deep-sea pelagic sediments belonging to the ophiolitic mélange units along northern branch of the Neotethys (İzmir-Ankara-Erzincan Suture Zone) in northern Turkey. In the Tafak region (Dursunbey, Balıkesir), Mn-deposit is currently mined from large- to medium- scale lenses (ca. 10 × 100 m) and interlayers with the mudstone and silicious pelagic sediments. This deposit comprises dominantly mineral assemblages of braunite, pyrolusite, and ganque minerals are quartz and rarely calcite. High Mn/Fe (437), Co/Zn (1.36), Co/Ni (2.04) ratios, low contents of ΣREE (27.7 ppm), Cu+Ni+Co (303 ppm), and also negative Ce anomaly (Ce/Ce*
PAAS
= 0.46), positive Y anomaly (Y
SN
/Ho
SN
= 1.33) with Y/Ho ratio (36.09) suggest that Tafak Mn deposit formed in a submarine hydrothermal system. Redox-sensitive element ratios (Ni/Co = 0.23-1.45, V/Mo = 2.63–20.81), positive Mn*
SN
(3.03–5.04), low Sr concentrations (82.2 ppm) and Ce
anom.
(− 0.52) values indicate that the Tafak Mn deposit was formed in low-salinity and oxygenated marine environment. Meanwhile, the presence of weakly negative Eu anomaly (0.94), Ce anomaly (0.46), and ΣREE/Fe ratio (127.8 x10
-4
) suggests that low-temperature hydrothermal fluids (< 200 °C) in pelagic depositional site of the İzmir-Ankara-Erzincan Neotethyan Ocean were effective in formation of the Tafak manganese deposit. |
| doi_str_mv | 10.1007/s12517-021-08576-0 |
| format | Article |
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PAAS
= 0.46), positive Y anomaly (Y
SN
/Ho
SN
= 1.33) with Y/Ho ratio (36.09) suggest that Tafak Mn deposit formed in a submarine hydrothermal system. Redox-sensitive element ratios (Ni/Co = 0.23-1.45, V/Mo = 2.63–20.81), positive Mn*
SN
(3.03–5.04), low Sr concentrations (82.2 ppm) and Ce
anom.
(− 0.52) values indicate that the Tafak Mn deposit was formed in low-salinity and oxygenated marine environment. Meanwhile, the presence of weakly negative Eu anomaly (0.94), Ce anomaly (0.46), and ΣREE/Fe ratio (127.8 x10
-4
) suggests that low-temperature hydrothermal fluids (< 200 °C) in pelagic depositional site of the İzmir-Ankara-Erzincan Neotethyan Ocean were effective in formation of the Tafak manganese deposit.</description><identifier>ISSN: 1866-7511</identifier><identifier>EISSN: 1866-7538</identifier><identifier>DOI: 10.1007/s12517-021-08576-0</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Calcite ; Chert ; Deep sea ; Deep water ; Earth and Environmental Science ; Earth science ; Earth Sciences ; Fluids ; Hydrothermal systems ; Interlayers ; Iron ; Low temperature ; Manganese ; Manganese deposits ; Marine environment ; Mineral assemblages ; Minerals ; Molybdenum ; Mudstone ; Nickel ; Ophiolites ; Original Paper ; Oxidoreductions ; Pelagic sediments ; Pyrolusite ; Ratios ; Sediments ; Zinc</subject><ispartof>Arabian journal of geosciences, 2021-11, Vol.14 (22), Article 2321</ispartof><rights>Saudi Society for Geosciences 2021</rights><rights>Saudi Society for Geosciences 2021.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a2938-41a47b027d78a2d776d115a952ca873be03f88f4f494f0d821bccae02fd4ce163</citedby><cites>FETCH-LOGICAL-a2938-41a47b027d78a2d776d115a952ca873be03f88f4f494f0d821bccae02fd4ce163</cites><orcidid>0000-0003-2478-8632</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12517-021-08576-0$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12517-021-08576-0$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids></links><search><creatorcontrib>Selman, Aydoğan M</creatorcontrib><title>The Tafak manganese deposit (Dursunbey-Balıkesir, NW Turkey): implications for the submarine hydrothermal origin of İzmir-Ankara-Erzincan Neotethyan Ocean</title><title>Arabian journal of geosciences</title><addtitle>Arab J Geosci</addtitle><description>In Turkey, radiolarian chert-hosted Mn-oxide deposits are exposed commonly within the deep-sea pelagic sediments belonging to the ophiolitic mélange units along northern branch of the Neotethys (İzmir-Ankara-Erzincan Suture Zone) in northern Turkey. In the Tafak region (Dursunbey, Balıkesir), Mn-deposit is currently mined from large- to medium- scale lenses (ca. 10 × 100 m) and interlayers with the mudstone and silicious pelagic sediments. This deposit comprises dominantly mineral assemblages of braunite, pyrolusite, and ganque minerals are quartz and rarely calcite. High Mn/Fe (437), Co/Zn (1.36), Co/Ni (2.04) ratios, low contents of ΣREE (27.7 ppm), Cu+Ni+Co (303 ppm), and also negative Ce anomaly (Ce/Ce*
PAAS
= 0.46), positive Y anomaly (Y
SN
/Ho
SN
= 1.33) with Y/Ho ratio (36.09) suggest that Tafak Mn deposit formed in a submarine hydrothermal system. Redox-sensitive element ratios (Ni/Co = 0.23-1.45, V/Mo = 2.63–20.81), positive Mn*
SN
(3.03–5.04), low Sr concentrations (82.2 ppm) and Ce
anom.
(− 0.52) values indicate that the Tafak Mn deposit was formed in low-salinity and oxygenated marine environment. Meanwhile, the presence of weakly negative Eu anomaly (0.94), Ce anomaly (0.46), and ΣREE/Fe ratio (127.8 x10
-4
) suggests that low-temperature hydrothermal fluids (< 200 °C) in pelagic depositional site of the İzmir-Ankara-Erzincan Neotethyan Ocean were effective in formation of the Tafak manganese deposit.</description><subject>Calcite</subject><subject>Chert</subject><subject>Deep sea</subject><subject>Deep water</subject><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Fluids</subject><subject>Hydrothermal systems</subject><subject>Interlayers</subject><subject>Iron</subject><subject>Low temperature</subject><subject>Manganese</subject><subject>Manganese deposits</subject><subject>Marine environment</subject><subject>Mineral assemblages</subject><subject>Minerals</subject><subject>Molybdenum</subject><subject>Mudstone</subject><subject>Nickel</subject><subject>Ophiolites</subject><subject>Original Paper</subject><subject>Oxidoreductions</subject><subject>Pelagic sediments</subject><subject>Pyrolusite</subject><subject>Ratios</subject><subject>Sediments</subject><subject>Zinc</subject><issn>1866-7511</issn><issn>1866-7538</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp9kU1uFDEQhVuISITABVhZYgMSBtv9Yze7EMKPFCWbQSyt6u7yjDPT9lDuXnTOwiHIHXIwDIPILqt6Kr33SqWvKF5I8VYKod8lqWqpuVCSC1PrhotHxbE0TcN1XZrH_7WUT4qnKV0L0RihzXHxc7VBtgIHWzZCWEPAhGzAfUx-Yq8-zpTm0OHCP8Du7naLydMbdvmdrWba4vL6PfPjfud7mHwMiblIbMp9ae5GIB-QbZaBYl7RCDsWya99YNGxu183oyd-GrZAwM_pxoceArvEOOG0WbK86hHCs-LIwS7h83_zpPj26Xx19oVfXH3-enZ6wUG1peGVhEp3QulBG1CD1s0gZQ1trXowuuxQlM4YV7mqrZwYjJJd3wMK5YaqR9mUJ8XLQ--e4o8Z02Sv40whn7SqbstGaVG12aUOrp5iSoTO7snnPxcrhf1DwR4o2EzB_qVgRQ6Vh1DK5rBGuq9-IPUbnReOTQ</recordid><startdate>20211101</startdate><enddate>20211101</enddate><creator>Selman, Aydoğan M</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0003-2478-8632</orcidid></search><sort><creationdate>20211101</creationdate><title>The Tafak manganese deposit (Dursunbey-Balıkesir, NW Turkey): implications for the submarine hydrothermal origin of İzmir-Ankara-Erzincan Neotethyan Ocean</title><author>Selman, Aydoğan M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a2938-41a47b027d78a2d776d115a952ca873be03f88f4f494f0d821bccae02fd4ce163</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Calcite</topic><topic>Chert</topic><topic>Deep sea</topic><topic>Deep water</topic><topic>Earth and Environmental Science</topic><topic>Earth science</topic><topic>Earth Sciences</topic><topic>Fluids</topic><topic>Hydrothermal systems</topic><topic>Interlayers</topic><topic>Iron</topic><topic>Low temperature</topic><topic>Manganese</topic><topic>Manganese deposits</topic><topic>Marine environment</topic><topic>Mineral assemblages</topic><topic>Minerals</topic><topic>Molybdenum</topic><topic>Mudstone</topic><topic>Nickel</topic><topic>Ophiolites</topic><topic>Original Paper</topic><topic>Oxidoreductions</topic><topic>Pelagic sediments</topic><topic>Pyrolusite</topic><topic>Ratios</topic><topic>Sediments</topic><topic>Zinc</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Selman, Aydoğan M</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Arabian journal of geosciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Selman, Aydoğan M</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Tafak manganese deposit (Dursunbey-Balıkesir, NW Turkey): implications for the submarine hydrothermal origin of İzmir-Ankara-Erzincan Neotethyan Ocean</atitle><jtitle>Arabian journal of geosciences</jtitle><stitle>Arab J Geosci</stitle><date>2021-11-01</date><risdate>2021</risdate><volume>14</volume><issue>22</issue><artnum>2321</artnum><issn>1866-7511</issn><eissn>1866-7538</eissn><abstract>In Turkey, radiolarian chert-hosted Mn-oxide deposits are exposed commonly within the deep-sea pelagic sediments belonging to the ophiolitic mélange units along northern branch of the Neotethys (İzmir-Ankara-Erzincan Suture Zone) in northern Turkey. In the Tafak region (Dursunbey, Balıkesir), Mn-deposit is currently mined from large- to medium- scale lenses (ca. 10 × 100 m) and interlayers with the mudstone and silicious pelagic sediments. This deposit comprises dominantly mineral assemblages of braunite, pyrolusite, and ganque minerals are quartz and rarely calcite. High Mn/Fe (437), Co/Zn (1.36), Co/Ni (2.04) ratios, low contents of ΣREE (27.7 ppm), Cu+Ni+Co (303 ppm), and also negative Ce anomaly (Ce/Ce*
PAAS
= 0.46), positive Y anomaly (Y
SN
/Ho
SN
= 1.33) with Y/Ho ratio (36.09) suggest that Tafak Mn deposit formed in a submarine hydrothermal system. Redox-sensitive element ratios (Ni/Co = 0.23-1.45, V/Mo = 2.63–20.81), positive Mn*
SN
(3.03–5.04), low Sr concentrations (82.2 ppm) and Ce
anom.
(− 0.52) values indicate that the Tafak Mn deposit was formed in low-salinity and oxygenated marine environment. Meanwhile, the presence of weakly negative Eu anomaly (0.94), Ce anomaly (0.46), and ΣREE/Fe ratio (127.8 x10
-4
) suggests that low-temperature hydrothermal fluids (< 200 °C) in pelagic depositional site of the İzmir-Ankara-Erzincan Neotethyan Ocean were effective in formation of the Tafak manganese deposit.</abstract><cop>Cham</cop><pub>Springer International Publishing</pub><doi>10.1007/s12517-021-08576-0</doi><orcidid>https://orcid.org/0000-0003-2478-8632</orcidid></addata></record> |
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| language | eng |
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| subjects | Calcite Chert Deep sea Deep water Earth and Environmental Science Earth science Earth Sciences Fluids Hydrothermal systems Interlayers Iron Low temperature Manganese Manganese deposits Marine environment Mineral assemblages Minerals Molybdenum Mudstone Nickel Ophiolites Original Paper Oxidoreductions Pelagic sediments Pyrolusite Ratios Sediments Zinc |
| title | The Tafak manganese deposit (Dursunbey-Balıkesir, NW Turkey): implications for the submarine hydrothermal origin of İzmir-Ankara-Erzincan Neotethyan Ocean |
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