Geochemical constraints on petrogenesis of Late Cretaceous alkaline magmatism in east-central Anatolia (Hasancelebi–Basören, Malatya), Turkey
Late Cretaceous alkali magmatic rocks occur widely in the Hasancelebi and Basören regions (Malatya). The Hasancelebi and Basören intrusive rocks are mainly peralkaline and alkaline-oversaturated. The Hasancelebi intrusive rocks are made up of syenite to quartz monzonite. On the other hand the Basöre...
Gespeichert in:
| Veröffentlicht in: | Mineralogy and petrology 2009, Vol.95 (1-2), p.71-85 |
|---|---|
| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 85 |
|---|---|
| container_issue | 1-2 |
| container_start_page | 71 |
| container_title | Mineralogy and petrology |
| container_volume | 95 |
| creator | Ozgenc, I. Ilbeyli, N. |
| description | Late Cretaceous alkali magmatic rocks occur widely in the Hasancelebi and Basören regions (Malatya). The Hasancelebi and Basören intrusive rocks are mainly peralkaline and alkaline-oversaturated. The Hasancelebi intrusive rocks are made up of syenite to quartz monzonite. On the other hand the Basören intrusive rocks mainly contain feldspathoidal syenites that are cut by feldspathoid-bearing dykes. The Hasancelebi intrusive rocks show comparable field, petrographic and geochemical characteristics with A-type rocks. All intrusive rocks show enrichment in LILE and LREE relative to HFSE. The Th/Yb versus Ta/Yb diagram indicates that all magmatic rocks formed from an enriched mantle source region(s). The parental magma for the Basören rocks has a higher intraplate component than that from the Hasancelebi rocks which could be attributed to mantle source heterogeneity before collision in east-central Anatolia. Either delamination of the thermal boundary layer or slab-breakoff are likely mechanisms for the initiation of post-collisional magmatism in the Hasancelebi–Basören areas. |
| doi_str_mv | 10.1007/s00710-008-0027-0 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_304925362</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2038749251</sourcerecordid><originalsourceid>FETCH-LOGICAL-a338t-e7d1dc950fcfd76f26c45e05c627aca26ede7e7ad59850e4cf602119d6c3abf3</originalsourceid><addsrcrecordid>eNp1kM9KAzEQxoMoWKsP4C14UnB1stv9d6xFrVDx0nsYs7M1djepSXrozUcQfBdfwDfxSYxU8ORhZhjm-76BH2PHAi4EQHnpYxOQAFSx0jKBHTYQo6xKhCiqXTaAOovXEqp9duD9M0RhXokBe7slq56o1wo7rqzxwaE2wXNr-IqCswsy5HXcWz7DQHziKKAiu_YcuyV22hDvcdFj0L7n2nBCHxJFJgZ1fGww2E4jP52iR6Ooo0f99fp-hf7zw5E55_fYYdjg2Tmfr92SNodsr8XO09HvHLL5zfV8Mk1mD7d3k_EswSyrQkJlIxpV59CqtimLNi3UKCfIVZGWqDAtqKGSSmzyusqBRqotIBWibgqV4WObDdnJNnbl7MuafJDPdu1M_CgzGNVpnhVpFImtSDnrvaNWrpzu0W2kAPmDXW6xy0hT_mCXED3p1uOj1izI_QX_b_oGthSJ4A</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>304925362</pqid></control><display><type>article</type><title>Geochemical constraints on petrogenesis of Late Cretaceous alkaline magmatism in east-central Anatolia (Hasancelebi–Basören, Malatya), Turkey</title><source>SpringerLink</source><creator>Ozgenc, I. ; Ilbeyli, N.</creator><creatorcontrib>Ozgenc, I. ; Ilbeyli, N.</creatorcontrib><description>Late Cretaceous alkali magmatic rocks occur widely in the Hasancelebi and Basören regions (Malatya). The Hasancelebi and Basören intrusive rocks are mainly peralkaline and alkaline-oversaturated. The Hasancelebi intrusive rocks are made up of syenite to quartz monzonite. On the other hand the Basören intrusive rocks mainly contain feldspathoidal syenites that are cut by feldspathoid-bearing dykes. The Hasancelebi intrusive rocks show comparable field, petrographic and geochemical characteristics with A-type rocks. All intrusive rocks show enrichment in LILE and LREE relative to HFSE. The Th/Yb versus Ta/Yb diagram indicates that all magmatic rocks formed from an enriched mantle source region(s). The parental magma for the Basören rocks has a higher intraplate component than that from the Hasancelebi rocks which could be attributed to mantle source heterogeneity before collision in east-central Anatolia. Either delamination of the thermal boundary layer or slab-breakoff are likely mechanisms for the initiation of post-collisional magmatism in the Hasancelebi–Basören areas.</description><identifier>ISSN: 0930-0708</identifier><identifier>EISSN: 1438-1168</identifier><identifier>DOI: 10.1007/s00710-008-0027-0</identifier><language>eng</language><publisher>Vienna: Springer Vienna</publisher><subject>Alkalinity ; Boundary layers ; Cretaceous ; Earth and Environmental Science ; Earth Sciences ; Geochemistry ; Heterogeneity ; Inorganic Chemistry ; Magma ; Mineralogy ; Original Paper ; Petrochemicals ; Rocks</subject><ispartof>Mineralogy and petrology, 2009, Vol.95 (1-2), p.71-85</ispartof><rights>Springer-Verlag 2008</rights><rights>Springer-Verlag 2009</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a338t-e7d1dc950fcfd76f26c45e05c627aca26ede7e7ad59850e4cf602119d6c3abf3</citedby><cites>FETCH-LOGICAL-a338t-e7d1dc950fcfd76f26c45e05c627aca26ede7e7ad59850e4cf602119d6c3abf3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00710-008-0027-0$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00710-008-0027-0$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids></links><search><creatorcontrib>Ozgenc, I.</creatorcontrib><creatorcontrib>Ilbeyli, N.</creatorcontrib><title>Geochemical constraints on petrogenesis of Late Cretaceous alkaline magmatism in east-central Anatolia (Hasancelebi–Basören, Malatya), Turkey</title><title>Mineralogy and petrology</title><addtitle>Miner Petrol</addtitle><description>Late Cretaceous alkali magmatic rocks occur widely in the Hasancelebi and Basören regions (Malatya). The Hasancelebi and Basören intrusive rocks are mainly peralkaline and alkaline-oversaturated. The Hasancelebi intrusive rocks are made up of syenite to quartz monzonite. On the other hand the Basören intrusive rocks mainly contain feldspathoidal syenites that are cut by feldspathoid-bearing dykes. The Hasancelebi intrusive rocks show comparable field, petrographic and geochemical characteristics with A-type rocks. All intrusive rocks show enrichment in LILE and LREE relative to HFSE. The Th/Yb versus Ta/Yb diagram indicates that all magmatic rocks formed from an enriched mantle source region(s). The parental magma for the Basören rocks has a higher intraplate component than that from the Hasancelebi rocks which could be attributed to mantle source heterogeneity before collision in east-central Anatolia. Either delamination of the thermal boundary layer or slab-breakoff are likely mechanisms for the initiation of post-collisional magmatism in the Hasancelebi–Basören areas.</description><subject>Alkalinity</subject><subject>Boundary layers</subject><subject>Cretaceous</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geochemistry</subject><subject>Heterogeneity</subject><subject>Inorganic Chemistry</subject><subject>Magma</subject><subject>Mineralogy</subject><subject>Original Paper</subject><subject>Petrochemicals</subject><subject>Rocks</subject><issn>0930-0708</issn><issn>1438-1168</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2009</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp1kM9KAzEQxoMoWKsP4C14UnB1stv9d6xFrVDx0nsYs7M1djepSXrozUcQfBdfwDfxSYxU8ORhZhjm-76BH2PHAi4EQHnpYxOQAFSx0jKBHTYQo6xKhCiqXTaAOovXEqp9duD9M0RhXokBe7slq56o1wo7rqzxwaE2wXNr-IqCswsy5HXcWz7DQHziKKAiu_YcuyV22hDvcdFj0L7n2nBCHxJFJgZ1fGww2E4jP52iR6Ooo0f99fp-hf7zw5E55_fYYdjg2Tmfr92SNodsr8XO09HvHLL5zfV8Mk1mD7d3k_EswSyrQkJlIxpV59CqtimLNi3UKCfIVZGWqDAtqKGSSmzyusqBRqotIBWibgqV4WObDdnJNnbl7MuafJDPdu1M_CgzGNVpnhVpFImtSDnrvaNWrpzu0W2kAPmDXW6xy0hT_mCXED3p1uOj1izI_QX_b_oGthSJ4A</recordid><startdate>2009</startdate><enddate>2009</enddate><creator>Ozgenc, I.</creator><creator>Ilbeyli, N.</creator><general>Springer Vienna</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7XB</scope><scope>88I</scope><scope>8BQ</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H96</scope><scope>HCIFZ</scope><scope>JG9</scope><scope>KB.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope></search><sort><creationdate>2009</creationdate><title>Geochemical constraints on petrogenesis of Late Cretaceous alkaline magmatism in east-central Anatolia (Hasancelebi–Basören, Malatya), Turkey</title><author>Ozgenc, I. ; Ilbeyli, N.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a338t-e7d1dc950fcfd76f26c45e05c627aca26ede7e7ad59850e4cf602119d6c3abf3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2009</creationdate><topic>Alkalinity</topic><topic>Boundary layers</topic><topic>Cretaceous</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geochemistry</topic><topic>Heterogeneity</topic><topic>Inorganic Chemistry</topic><topic>Magma</topic><topic>Mineralogy</topic><topic>Original Paper</topic><topic>Petrochemicals</topic><topic>Rocks</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ozgenc, I.</creatorcontrib><creatorcontrib>Ilbeyli, N.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</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>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Materials Science Collection</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</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>ProQuest Research Library</collection><collection>ProQuest Science Journals</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Environmental Science 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>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Mineralogy and petrology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ozgenc, I.</au><au>Ilbeyli, N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geochemical constraints on petrogenesis of Late Cretaceous alkaline magmatism in east-central Anatolia (Hasancelebi–Basören, Malatya), Turkey</atitle><jtitle>Mineralogy and petrology</jtitle><stitle>Miner Petrol</stitle><date>2009</date><risdate>2009</risdate><volume>95</volume><issue>1-2</issue><spage>71</spage><epage>85</epage><pages>71-85</pages><issn>0930-0708</issn><eissn>1438-1168</eissn><abstract>Late Cretaceous alkali magmatic rocks occur widely in the Hasancelebi and Basören regions (Malatya). The Hasancelebi and Basören intrusive rocks are mainly peralkaline and alkaline-oversaturated. The Hasancelebi intrusive rocks are made up of syenite to quartz monzonite. On the other hand the Basören intrusive rocks mainly contain feldspathoidal syenites that are cut by feldspathoid-bearing dykes. The Hasancelebi intrusive rocks show comparable field, petrographic and geochemical characteristics with A-type rocks. All intrusive rocks show enrichment in LILE and LREE relative to HFSE. The Th/Yb versus Ta/Yb diagram indicates that all magmatic rocks formed from an enriched mantle source region(s). The parental magma for the Basören rocks has a higher intraplate component than that from the Hasancelebi rocks which could be attributed to mantle source heterogeneity before collision in east-central Anatolia. Either delamination of the thermal boundary layer or slab-breakoff are likely mechanisms for the initiation of post-collisional magmatism in the Hasancelebi–Basören areas.</abstract><cop>Vienna</cop><pub>Springer Vienna</pub><doi>10.1007/s00710-008-0027-0</doi><tpages>15</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0930-0708 |
| ispartof | Mineralogy and petrology, 2009, Vol.95 (1-2), p.71-85 |
| issn | 0930-0708 1438-1168 |
| language | eng |
| recordid | cdi_proquest_journals_304925362 |
| source | SpringerLink |
| subjects | Alkalinity Boundary layers Cretaceous Earth and Environmental Science Earth Sciences Geochemistry Heterogeneity Inorganic Chemistry Magma Mineralogy Original Paper Petrochemicals Rocks |
| title | Geochemical constraints on petrogenesis of Late Cretaceous alkaline magmatism in east-central Anatolia (Hasancelebi–Basören, Malatya), Turkey |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-10T18%3A44%3A34IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Geochemical%20constraints%20on%20petrogenesis%20of%20Late%20Cretaceous%20alkaline%20magmatism%20in%20east-central%20Anatolia%20(Hasancelebi%E2%80%93Bas%C3%B6ren,%20Malatya),%20Turkey&rft.jtitle=Mineralogy%20and%20petrology&rft.au=Ozgenc,%20I.&rft.date=2009&rft.volume=95&rft.issue=1-2&rft.spage=71&rft.epage=85&rft.pages=71-85&rft.issn=0930-0708&rft.eissn=1438-1168&rft_id=info:doi/10.1007/s00710-008-0027-0&rft_dat=%3Cproquest_cross%3E2038749251%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=304925362&rft_id=info:pmid/&rfr_iscdi=true |