Petrogenesis and geodynamics of plagiogranites from Central Turkey (Ekecikdağ/Aksaray): new geochemical and isotopic data for generation in an arc basin system within the northern branch of Neotethys
In the Late Cretaceous, throughout the closure of the Neotethys Ocean, ophiolitic rocks from the İzmir–Ankara–Erzincan ocean branch were overthrusted the northern margin of the Tauride-Anatolide Platform. The ophiolitic rocks in the Ekecikdağ (Aksaray/Central Turkey) region typify the oceanic crust...
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| Veröffentlicht in: | International journal of earth sciences : Geologische Rundschau 2017-06, Vol.106 (4), p.1181-1203 |
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| creator | Köksal, Serhat Toksoy-Köksal, Fatma Göncüoglu, M. Cemal |
| description | In the Late Cretaceous, throughout the closure of the Neotethys Ocean, ophiolitic rocks from the İzmir–Ankara–Erzincan ocean branch were overthrusted the northern margin of the Tauride-Anatolide Platform. The ophiolitic rocks in the Ekecikdağ (Aksaray/Central Turkey) region typify the oceanic crust of the İzmir–Ankara–Erzincan branch of Neotethys. The gabbros in the area are cut by copious plagiogranite dykes, and both rock units are intruded by mafic dykes. The plagiogranites are leucocratic, fine- to medium-grained calc-alkaline rocks characterized mainly by plagioclase and quartz, with minor amounts of biotite, hornblende and clinopyroxene, and accessory phases of zircon, titanite, apatite and opaque minerals. They are tonalite and trondhjemite in composition with high SiO
2
(69.9–75.9 wt%) and exceptionally low K
2
O ( |
| doi_str_mv | 10.1007/s00531-016-1401-5 |
| format | Article |
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2
(69.9–75.9 wt%) and exceptionally low K
2
O (<0.5 wt%) contents. The plagiogranites in common with gabbros and mafic dykes show high large-ion lithophile elements/high-field strength element ratios with depletion in Nb, Ti and light rare-earth elements with respect to N-MORB. The plagiogranites together with gabbros and mafic dykes show low initial
87
Sr/
86
Sr ratios (0.70419–0.70647), high ƐNd
(
T
)
(6.0–7.5) values with
206
Pb/
204
Pb (18.199–18.581),
207
Pb/
204
Pb (15.571–15.639) and
208
Pb/
204
Pb (38.292–38.605) ratios indicating a depleted mantle source modified with a subduction component. They show similar isotopic characteristics to the other supra-subduction zone (SSZ) ophiolites in the Eastern Mediterranean to East Anatolian–Lesser Caucasus and Iran regions. It is suggested that the Ekecikdağ plagiogranite was generated in a short time interval from a depleted mantle source in a SSZ/fore-arc basin setting, and its nature was further modified by a subduction component during intra-oceanic subduction.</description><identifier>ISSN: 1437-3254</identifier><identifier>EISSN: 1437-3262</identifier><identifier>DOI: 10.1007/s00531-016-1401-5</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Apatite ; Basins ; Biotite ; Composition ; Cretaceous ; Data analysis ; Depletion ; Earth ; Earth and Environmental Science ; Earth Sciences ; Field strength ; Gabbros ; Geochemistry ; Geodynamics ; Geology ; Geophysics/Geodesy ; Isotopes ; Lead isotopes ; Magma ; Mantle ; Mineral Resources ; Minerals ; Oceanic crust ; Oceans ; Ophiolites ; Original Paper ; Petrogenesis ; Plagioclase ; Rare earth elements ; Ratios ; Rock ; Rock intrusions ; Rocks ; Sedimentology ; Silica ; Silicon dioxide ; Strontium 87 ; Strontium isotopes ; Structural Geology ; Subduction ; Subduction zones ; Tectonophysics ; Titanite ; Titanium ; Zircon</subject><ispartof>International journal of earth sciences : Geologische Rundschau, 2017-06, Vol.106 (4), p.1181-1203</ispartof><rights>Springer-Verlag Berlin Heidelberg 2016</rights><rights>International Journal of Earth Sciences is a copyright of Springer, 2017.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-9e8e18dc513a70e9616e7987baed1360498f996ebfb963bd128cf40540a479753</citedby><cites>FETCH-LOGICAL-a339t-9e8e18dc513a70e9616e7987baed1360498f996ebfb963bd128cf40540a479753</cites><orcidid>0000-0002-0094-9481</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/s00531-016-1401-5$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00531-016-1401-5$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Köksal, Serhat</creatorcontrib><creatorcontrib>Toksoy-Köksal, Fatma</creatorcontrib><creatorcontrib>Göncüoglu, M. Cemal</creatorcontrib><title>Petrogenesis and geodynamics of plagiogranites from Central Turkey (Ekecikdağ/Aksaray): new geochemical and isotopic data for generation in an arc basin system within the northern branch of Neotethys</title><title>International journal of earth sciences : Geologische Rundschau</title><addtitle>Int J Earth Sci (Geol Rundsch)</addtitle><description>In the Late Cretaceous, throughout the closure of the Neotethys Ocean, ophiolitic rocks from the İzmir–Ankara–Erzincan ocean branch were overthrusted the northern margin of the Tauride-Anatolide Platform. The ophiolitic rocks in the Ekecikdağ (Aksaray/Central Turkey) region typify the oceanic crust of the İzmir–Ankara–Erzincan branch of Neotethys. The gabbros in the area are cut by copious plagiogranite dykes, and both rock units are intruded by mafic dykes. The plagiogranites are leucocratic, fine- to medium-grained calc-alkaline rocks characterized mainly by plagioclase and quartz, with minor amounts of biotite, hornblende and clinopyroxene, and accessory phases of zircon, titanite, apatite and opaque minerals. They are tonalite and trondhjemite in composition with high SiO
2
(69.9–75.9 wt%) and exceptionally low K
2
O (<0.5 wt%) contents. The plagiogranites in common with gabbros and mafic dykes show high large-ion lithophile elements/high-field strength element ratios with depletion in Nb, Ti and light rare-earth elements with respect to N-MORB. The plagiogranites together with gabbros and mafic dykes show low initial
87
Sr/
86
Sr ratios (0.70419–0.70647), high ƐNd
(
T
)
(6.0–7.5) values with
206
Pb/
204
Pb (18.199–18.581),
207
Pb/
204
Pb (15.571–15.639) and
208
Pb/
204
Pb (38.292–38.605) ratios indicating a depleted mantle source modified with a subduction component. They show similar isotopic characteristics to the other supra-subduction zone (SSZ) ophiolites in the Eastern Mediterranean to East Anatolian–Lesser Caucasus and Iran regions. It is suggested that the Ekecikdağ plagiogranite was generated in a short time interval from a depleted mantle source in a SSZ/fore-arc basin setting, and its nature was further modified by a subduction component during intra-oceanic subduction.</description><subject>Apatite</subject><subject>Basins</subject><subject>Biotite</subject><subject>Composition</subject><subject>Cretaceous</subject><subject>Data analysis</subject><subject>Depletion</subject><subject>Earth</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Field strength</subject><subject>Gabbros</subject><subject>Geochemistry</subject><subject>Geodynamics</subject><subject>Geology</subject><subject>Geophysics/Geodesy</subject><subject>Isotopes</subject><subject>Lead isotopes</subject><subject>Magma</subject><subject>Mantle</subject><subject>Mineral Resources</subject><subject>Minerals</subject><subject>Oceanic crust</subject><subject>Oceans</subject><subject>Ophiolites</subject><subject>Original Paper</subject><subject>Petrogenesis</subject><subject>Plagioclase</subject><subject>Rare earth elements</subject><subject>Ratios</subject><subject>Rock</subject><subject>Rock intrusions</subject><subject>Rocks</subject><subject>Sedimentology</subject><subject>Silica</subject><subject>Silicon dioxide</subject><subject>Strontium 87</subject><subject>Strontium isotopes</subject><subject>Structural Geology</subject><subject>Subduction</subject><subject>Subduction zones</subject><subject>Tectonophysics</subject><subject>Titanite</subject><subject>Titanium</subject><subject>Zircon</subject><issn>1437-3254</issn><issn>1437-3262</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp1kctuFDEQRVuISITAB7AriQ0smtj9NrtoFB5SRLIIa6vaXd3tzIw9lD2K-mv4mSz4LNwahNiwqofuPVXSzbI3UnyQQrSXQYi6lLmQTS4rIfP6WXYuq7LNy6Ipnv_t6-pF9jKEByHWhTzPft1RZD-Ro2ADoBtgIj8sDvfWBPAjHHY4WT8xOhspwMh-DxtykXEH90fe0gLvrrdk7HbAp5-XV9uAjMv7j-DocWWZmRIqiVe2DT76gzUwYEQYPcN6mTFa78C6pAFkAz2GNIQlRNrDo41zmuJM4Dynwg769I6Z1_e-kY8U5yW8ys5G3AV6_adeZN8_Xd9vvuQ3t5-_bq5ucixLFXNFHcluMLUssRWkGtlQq7q2Rxpk2YhKdaNSDfVjr5qyH2TRmbESdSWwalVblxfZ2xP3wP7HkULUD_7ILp3UskvOoqvbLqnkSWXYh8A06gPbPfKipdBrYPoUmE6B6TUwvZKLkyckrZuI_yH_1_QbEOedJg</recordid><startdate>20170601</startdate><enddate>20170601</enddate><creator>Köksal, Serhat</creator><creator>Toksoy-Köksal, Fatma</creator><creator>Göncüoglu, M. Cemal</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</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>KL.</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><orcidid>https://orcid.org/0000-0002-0094-9481</orcidid></search><sort><creationdate>20170601</creationdate><title>Petrogenesis and geodynamics of plagiogranites from Central Turkey (Ekecikdağ/Aksaray): new geochemical and isotopic data for generation in an arc basin system within the northern branch of Neotethys</title><author>Köksal, Serhat ; Toksoy-Köksal, Fatma ; Göncüoglu, M. Cemal</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a339t-9e8e18dc513a70e9616e7987baed1360498f996ebfb963bd128cf40540a479753</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Apatite</topic><topic>Basins</topic><topic>Biotite</topic><topic>Composition</topic><topic>Cretaceous</topic><topic>Data analysis</topic><topic>Depletion</topic><topic>Earth</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Field strength</topic><topic>Gabbros</topic><topic>Geochemistry</topic><topic>Geodynamics</topic><topic>Geology</topic><topic>Geophysics/Geodesy</topic><topic>Isotopes</topic><topic>Lead isotopes</topic><topic>Magma</topic><topic>Mantle</topic><topic>Mineral Resources</topic><topic>Minerals</topic><topic>Oceanic crust</topic><topic>Oceans</topic><topic>Ophiolites</topic><topic>Original Paper</topic><topic>Petrogenesis</topic><topic>Plagioclase</topic><topic>Rare earth elements</topic><topic>Ratios</topic><topic>Rock</topic><topic>Rock intrusions</topic><topic>Rocks</topic><topic>Sedimentology</topic><topic>Silica</topic><topic>Silicon dioxide</topic><topic>Strontium 87</topic><topic>Strontium isotopes</topic><topic>Structural Geology</topic><topic>Subduction</topic><topic>Subduction zones</topic><topic>Tectonophysics</topic><topic>Titanite</topic><topic>Titanium</topic><topic>Zircon</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Köksal, Serhat</creatorcontrib><creatorcontrib>Toksoy-Köksal, Fatma</creatorcontrib><creatorcontrib>Göncüoglu, M. 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Cemal</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Petrogenesis and geodynamics of plagiogranites from Central Turkey (Ekecikdağ/Aksaray): new geochemical and isotopic data for generation in an arc basin system within the northern branch of Neotethys</atitle><jtitle>International journal of earth sciences : Geologische Rundschau</jtitle><stitle>Int J Earth Sci (Geol Rundsch)</stitle><date>2017-06-01</date><risdate>2017</risdate><volume>106</volume><issue>4</issue><spage>1181</spage><epage>1203</epage><pages>1181-1203</pages><issn>1437-3254</issn><eissn>1437-3262</eissn><abstract>In the Late Cretaceous, throughout the closure of the Neotethys Ocean, ophiolitic rocks from the İzmir–Ankara–Erzincan ocean branch were overthrusted the northern margin of the Tauride-Anatolide Platform. The ophiolitic rocks in the Ekecikdağ (Aksaray/Central Turkey) region typify the oceanic crust of the İzmir–Ankara–Erzincan branch of Neotethys. The gabbros in the area are cut by copious plagiogranite dykes, and both rock units are intruded by mafic dykes. The plagiogranites are leucocratic, fine- to medium-grained calc-alkaline rocks characterized mainly by plagioclase and quartz, with minor amounts of biotite, hornblende and clinopyroxene, and accessory phases of zircon, titanite, apatite and opaque minerals. They are tonalite and trondhjemite in composition with high SiO
2
(69.9–75.9 wt%) and exceptionally low K
2
O (<0.5 wt%) contents. The plagiogranites in common with gabbros and mafic dykes show high large-ion lithophile elements/high-field strength element ratios with depletion in Nb, Ti and light rare-earth elements with respect to N-MORB. The plagiogranites together with gabbros and mafic dykes show low initial
87
Sr/
86
Sr ratios (0.70419–0.70647), high ƐNd
(
T
)
(6.0–7.5) values with
206
Pb/
204
Pb (18.199–18.581),
207
Pb/
204
Pb (15.571–15.639) and
208
Pb/
204
Pb (38.292–38.605) ratios indicating a depleted mantle source modified with a subduction component. They show similar isotopic characteristics to the other supra-subduction zone (SSZ) ophiolites in the Eastern Mediterranean to East Anatolian–Lesser Caucasus and Iran regions. It is suggested that the Ekecikdağ plagiogranite was generated in a short time interval from a depleted mantle source in a SSZ/fore-arc basin setting, and its nature was further modified by a subduction component during intra-oceanic subduction.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00531-016-1401-5</doi><tpages>23</tpages><orcidid>https://orcid.org/0000-0002-0094-9481</orcidid></addata></record> |
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| ispartof | International journal of earth sciences : Geologische Rundschau, 2017-06, Vol.106 (4), p.1181-1203 |
| issn | 1437-3254 1437-3262 |
| language | eng |
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| source | SpringerLink Journals |
| subjects | Apatite Basins Biotite Composition Cretaceous Data analysis Depletion Earth Earth and Environmental Science Earth Sciences Field strength Gabbros Geochemistry Geodynamics Geology Geophysics/Geodesy Isotopes Lead isotopes Magma Mantle Mineral Resources Minerals Oceanic crust Oceans Ophiolites Original Paper Petrogenesis Plagioclase Rare earth elements Ratios Rock Rock intrusions Rocks Sedimentology Silica Silicon dioxide Strontium 87 Strontium isotopes Structural Geology Subduction Subduction zones Tectonophysics Titanite Titanium Zircon |
| title | Petrogenesis and geodynamics of plagiogranites from Central Turkey (Ekecikdağ/Aksaray): new geochemical and isotopic data for generation in an arc basin system within the northern branch of Neotethys |
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