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Article: A review of the nature of magmatism in Central Anatolia during the mesozoic post-collisional period
Title | A review of the nature of magmatism in Central Anatolia during the mesozoic post-collisional period |
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Authors | |
Issue Date | 2001 |
Publisher | Taylor & Francis Inc. The Journal's web site is located at http://www.tandf.co.uk/journals/TIGR |
Citation | International Geology Review, 2001, v. 43 n. 8, p. 695-710 How to Cite? |
Abstract | Magmatism in central Anatolia is characterized by petrographically and chemically distinct granitic and syenitic rocks. The granitic magmatism comprises C-type (crustal-derived) and H-type (hybrid) monzogranites and monzonites. Garnet-bearing C-type leucogranites represent the oldest magmatic phase, but younger hornblende ± biotite ± K-feldspar H-type plutons dominate the geology of the Central Anatolian Crystalline Complex (CACC). These typically include mafic microgranular enclaves. The granitic magmatism predates syenitic intrusions, among which quartz-bearing syenites were emplaced prior to feldspathoid-bearing ones. The nature of magmatism in central Anatolia varies through time from peraluminous to metaluminous to alkaline. These different magma types reflect distinct stages of post-collisional magmatism, in which interaction between crust and mantle varied considerably. The C-type granites of the early stages of post-collisional magmatism were likely derived by partial melting of the lower continental crust induced by mafic magma underplating as a result of lithospheric delamination. The H-type granites and syenites of the mature and advanced stages of post-collisional magmatism indicate a significant contribution from mantle-derived magma within a continuous or episodic extensional tectonic regime. |
Persistent Identifier | http://hdl.handle.net/10722/178219 |
ISSN | 2023 Impact Factor: 2.1 2023 SCImago Journal Rankings: 0.927 |
ISI Accession Number ID | |
References |
DC Field | Value | Language |
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dc.contributor.author | DüzgörenAydin, NS | en_US |
dc.contributor.author | Malpas, J | en_US |
dc.contributor.author | Göncüoglu, MC | en_US |
dc.contributor.author | Erler, A | en_US |
dc.date.accessioned | 2012-12-19T09:43:29Z | - |
dc.date.available | 2012-12-19T09:43:29Z | - |
dc.date.issued | 2001 | en_US |
dc.identifier.citation | International Geology Review, 2001, v. 43 n. 8, p. 695-710 | en_US |
dc.identifier.issn | 0020-6814 | en_US |
dc.identifier.uri | http://hdl.handle.net/10722/178219 | - |
dc.description.abstract | Magmatism in central Anatolia is characterized by petrographically and chemically distinct granitic and syenitic rocks. The granitic magmatism comprises C-type (crustal-derived) and H-type (hybrid) monzogranites and monzonites. Garnet-bearing C-type leucogranites represent the oldest magmatic phase, but younger hornblende ± biotite ± K-feldspar H-type plutons dominate the geology of the Central Anatolian Crystalline Complex (CACC). These typically include mafic microgranular enclaves. The granitic magmatism predates syenitic intrusions, among which quartz-bearing syenites were emplaced prior to feldspathoid-bearing ones. The nature of magmatism in central Anatolia varies through time from peraluminous to metaluminous to alkaline. These different magma types reflect distinct stages of post-collisional magmatism, in which interaction between crust and mantle varied considerably. The C-type granites of the early stages of post-collisional magmatism were likely derived by partial melting of the lower continental crust induced by mafic magma underplating as a result of lithospheric delamination. The H-type granites and syenites of the mature and advanced stages of post-collisional magmatism indicate a significant contribution from mantle-derived magma within a continuous or episodic extensional tectonic regime. | en_US |
dc.language | eng | en_US |
dc.publisher | Taylor & Francis Inc. The Journal's web site is located at http://www.tandf.co.uk/journals/TIGR | en_US |
dc.relation.ispartof | International Geology Review | en_US |
dc.title | A review of the nature of magmatism in Central Anatolia during the mesozoic post-collisional period | en_US |
dc.type | Article | en_US |
dc.identifier.email | Malpas, J: jgmalpas@hku.hk | en_US |
dc.identifier.authority | Malpas, J=rp00059 | en_US |
dc.description.nature | link_to_subscribed_fulltext | en_US |
dc.identifier.doi | 10.1080/00206810109465042 | - |
dc.identifier.scopus | eid_2-s2.0-0035176317 | en_US |
dc.identifier.hkuros | 55591 | - |
dc.relation.references | http://www.scopus.com/mlt/select.url?eid=2-s2.0-0035176317&selection=ref&src=s&origin=recordpage | en_US |
dc.identifier.volume | 43 | en_US |
dc.identifier.issue | 8 | en_US |
dc.identifier.spage | 695 | en_US |
dc.identifier.epage | 710 | en_US |
dc.identifier.isi | WOS:000172227300004 | - |
dc.publisher.place | United States | en_US |
dc.identifier.scopusauthorid | DüzgörenAydin, NS=6602460166 | en_US |
dc.identifier.scopusauthorid | Malpas, J=7006136845 | en_US |
dc.identifier.scopusauthorid | Göncüoglu, MC=7003963764 | en_US |
dc.identifier.scopusauthorid | Erler, A=6601988853 | en_US |
dc.identifier.issnl | 0020-6814 | - |